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2025,99(2):297-319, DOI: 10.1111/1755-6724.15292
Abstract:
East Asian continental tectonics challenges the plate tectonics paradigm with its diffuse intraplate deformation, magmatism, and earthquakes. Despite extensive studies, fundamental questions persist. This review examines ten critical questions of East Asian tectonics, including the thickness of the continental lithosphere, the origin of the North–South Gravity Lineament, and the northern extent of the Indian plate beneath the Tibetan Plateau. Additional questions address the Tibetan Plateau's lateral growth, the Tianshan mountain building, the mantle flow in response to the Indo-Asian collision, and the formation of the Shanxi Rift. The review also explores the subduction along the eastern margins of the East Asian Continent and the origins of the Changbaishan volcanic field, the destruction of the North China Craton, and the development of the Mesozoic Large Granitic Province in South China. Originally presented at the DEEP2024 workshop to stimulate discussion of how SinoProbe-II research initiatives could advance our understanding of Asian tectonics, this review provides context for each question, summarizes current knowledge, and identifies promising research directions.
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YU Kaifeng,WU Wenhao,SUN Wei,CHEN Jun,WANG Xuri
2025,99(2):320-331, DOI: 10.1111/1755-6724.15288
Abstract:
Twelve new dinosaur teeth have recently been recovered from three localities in the Upper Cretaceous Nenjiang Formation of the Songliao Basin. Although fragmentary, the material offers enough evidence to identify the following taxa: tyrannosaurids, dromaeosaurines, velociraptorines, hadrosauroids, and titanosaurs. In addition to the previously known dinosaurs from the basin, several new ones have been identified, extending the paleogeographic range of related taxa. The discovery of these new fossil remains provides valuable insights into dinosaur diversity and sheds light on the terrestrial ecosystem during the Late Cretaceous in the Songliao Basin.
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Fikret GOKTAS,Serdar MAYDA,Mehmet Cihat ALCICEK
2025,99(2):332-351, DOI: 10.1111/1755-6724.15279
Abstract:
In a re-examination of the Neogene stratigraphy of the U?ak, Güre, and Selendi basins of western Anatolia, western Turkey, the stratigraphic position of the previously defined ?nay Group is revised, which was previously considered to be of the Middle Miocene age. Based on mammalian biochronology and stratigraphic relationships, two sequences are identified, separated by conformable/transitional contacts within the former group: the Middle Miocene Güre Group is composed of the Fak?l? Formation, characterized by alluvial fan deposits, and the lacustrine Derbent Formation. Radiometric dating of alkaline volcanics laterally associated with Güre Group sediments in the U?ak and Güre basins, and mammalian fossils re-evaluated into the MN5-6 biozones in the Selendi Basin, indicate early Middle Miocene. Considering the stratigraphic relationship with the overlying early Late Miocene ?nay Group as redefined, we estimate that the Güre Group was deposited in the Middle Miocene. The ?nay Group is characterized by a lateral–vertical transition from alluvial deposits of the Ahmetler Formation to the overlying lacustrine Ulubey Formation. An MN9-10 fauna, containing deinotheres, was found within the latter formation.
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2025,99(2):352-369, DOI: 10.1111/1755-6724.15282
Abstract:
The approximately 3000 km long Tan–Lu fault zone (TLFZ) in East Asia is the longest continental strike-slip fault zone in the world and exemplifies how such a fault zone forms and propagates on a continental scale. Structural and geochronological data from the TLFZ and surrounding regions indicate that the fault zone originated as NE/SW-striking sinistral ductile shear zones along an oblique continental convergence margin during the Triassic indentation collision between the North China Craton and the Yangtze Block. The Triassic fault zone, with a total length of about 720 km between the Dabie and Sulu orogens, exhibited an apparent sinistral offset of approximately 300 km along the TLFZ. The second stage of sinistral movement occurred in the earliest Late Jurassic, reactivating the pre-existing southern segment and propagating northwards to the southern coastline of present-day Bohai Bay, as well as forming a significant portion of the Dunhua–Mishan fault zone. The third stage of sinistral movement, in the earliest Early Cretaceous, was the most intense strike-slip movement of the Mesozoic, leading to the complete linkage of the TLFZ. This stage included further northward propagation of the southern–middle segment, both southward and northward propagation of the Dunhua–Mishan fault zone, as well as the formation of the entire Yilan–Yitong fault zone. The fourth stage, in the earliest Late Cretaceous, involved the reactivation of the entire TLFZ. Following its Triassic origin due to the indentation collision, the subduction of the Paleo-Pacific Plate and the subduction and closure of the Mongol–Okhotsk Ocean were responsible for the multi-stage sinistral movements from the Late Jurassic to the Cretaceous. The evolution of the TLFZ demonstrates that a continental-scale strike-slip fault zone (>1000 km long) forms through multiple stages of propagation and linkage in dynamic settings of plate convergence.
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Farid MAKROUM,Mohamed BADAWI,Kurt STUWE,Norbert NEMETH,Mahmoud ABDELATIF,Ahmed SHALABY
2025,99(2):370-393, DOI: 10.1111/1755-6724.15290
Abstract:
The Barud gneissic dome complex is situated along the ENE-trending dextral shear zone of the Qena–Safaga Line that serves as a significant tectonic boundary between the basement terrains of the Northern and Central Eastern Desert. These terrains exhibit distinct differences in crustal composition and deformation style. The Northern Eastern Desert and its extension into Sinai are predominantly composed of gneissic granites that are intruded by large batholiths of calc-alkaline and alkaline granites. Conversely, the Central and Southern Eastern Desert are commonly blanketed by a carapace of ophiolite-bearing volcano-sedimentary rocks of the Pan-African cover nappes. These northern terrains, just north of the Barud dome complex, the crust underwent significant NW–SE regional crustal extension across the Qena–Safaga Line, which sharply delineates the northern limit of the transpressional deformations linked to the Najd fault system in the Central and Southern Eastern Desert. Through comprehensive geological mapping and the integration of various geophysical, geochemical and geochronological data, this paper offers explanations for the contrasting geological features of the basement terrains on both sides of the Qena–Safaga Line and its analogous Fatira Shear Zone that plays a significant role in tectonic modeling of the Barud dome complex region. The Barud gneissic protolith experienced crustal shortening approximately 697 million years ago in the NW–SE direction, initiating dextral motion along the Fatira Shear Zone. Large batholiths of granodiorite/tonalite complex intruded the Barud gneissic dome protolith around 630 million years ago along the Qena–Safaga Line, at relatively shallow crustal depths, following the same orientation as the earlier shortening direction. Ongoing magmatic activity along the Qena–Safaga Line indicates intense magmatic underplating, resulting in significant intrusions of granodioritic melts into the early rifted crust of the Northern Eastern Desert and Sinai terrains. The crust of these northern terrains likely underwent isostatic compensation through uplifting and subsequent erosion. The disappearance of ophiolite-bearing belts and the presence of Paleo- to Mesoproterozoic continental-derived cobbles and ignimbrites in Sinai metasedimentary belts and Northern Eastern Desert molasse basins suggest that the northern terrains, located north of the Qena–Safaga Line, originated as a cohesive, thin continental crust that rifted off the eastern passive margin of the Sahara Metacraton during the early Neoproterozoic rifting of the Rodinia supercontinent.
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LONG Kangjie,FENG Qianqian,TENGER Borjigin,QIU Nansheng,YU Taiyan
2025,99(2):394-408, DOI: 10.1111/1755-6724.15287
Abstract:
Apatite (U-Th)/He and fission track dating and tectono-thermal history modeling were used to reconstruct the Meso–Cenozoic tectonic evolution of the Huangling paleo-uplift in the Middle Yangtze Block, South China. The tectono-thermal evolution showed different tectonic exhumation/subsidence processes in the tectonic evolution of the foreland basin. The apatite (U-Th)/He ages ranged from 31.3 to 77.8 Ma, recording the thermal events of the Cenozoic Himalayan movement and indicating progressive exhumation extending from the southeast to the northwest. The thermal information of the Mesozoic Yanshan movement period was recorded by the apatite fission track age with a pooled age of 93.8 to 147 Ma. The exhumation of the Huangling paleo-uplift began in the Late Jurassic. The tectono-thermal evolution was characterized by a rapid uplift during 140–115 Ma, subsidence during 115–60 Ma, a rapid uplift during 40–30 Ma, and a slow uplift from 30 Ma to the present. The western Hunan–Hubei Depression was exhumed in the Middle Jurassic, and the tectono-thermal evolution was characterized by a rapid uplift during 160–135 Ma, a slow uplift during 135–50 Ma, a rapid uplift during 50–25 Ma, and a slow uplift from 25 Ma to the present. This Cenozoic exhumation was a response to the far field effect of the eastward growth of the Tibetan Plateau. The Cretaceous basins exposed in the surrounding areas of the Huangling paleo-uplift (Zigui basin, Yichang slope, and Huaguoping synclinorium) are foreland basins formed by the bi-directional compression of the Qinling–Dabie orogenic belt and the Xuefengshan intracontinental deformation system.
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2025,99(2):409-424, DOI: 10.1111/1755-6724.15254
Abstract:
Fragments of Proto-Tethyan oceanic lithosphere are well-preserved along the southern belt of the North Qilian suture, and the origin and emplacement of these ophiolites have become subjects of intense debate. In this study, we integrate field observations, mineralogical and geochemical analyses, zircon U-Pb dating, and isotopic data to investigate the Yanglong ophiolite. The Yanglong ophiolitic rocks are found as tectonic slices resting on the Neoproterozoic sedimentary and volcanic rocks. These rocks are composed of Cambrian serpentinized peridotite, gabbro, dolerite, and rodingite. The spinels in the serpentinized peridotites have variable Cr# values (21, 38–46, and 59–61) and display affinity to those in abyssal and forearc peridotites. The dolerites show slight enrichment in Th and have elevated (La/Sm)N ratios (1.19–2.01), indicating a subduction-related geochemical affinity. The Yanglong ophiolitic rocks have positive zircon εHf(t) values (+10.3 to +18.4) and whole-rock εNd(t) values (+5.3 to +6.7) indicating derivation from partial melting of a depleted mantle source. These results, together with the regional geology, collectively suggest that the Yanglong ophiolite was generated in a forearc setting during the Early Cambrian northward intra-oceanic subduction. It was emplaced onto the Central Qilian Block during the subsequent arc–continent collision, no later than the Early Ordovician.
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2025,99(2):425-440, DOI: 10.1111/1755-6724.15284
Abstract:
The Qinling orogenic belt in central China underwent long-term tectonic evolution during an amalgamation between the North China and South China cratons. However, intense compressional deformation and uplift erosion resulted in the transformation and disappearance of much geological record from the Qinling orogenic belt, and the tectonic evolution of this belt remains poorly constrained during the Triassic. Located in the northernmost margin of the South China Craton, the Sichuan Basin preserves the complete Triassic sedimentary succession, and can provide significant information for understanding the Triassic tectonic evolution of the Qinling orogenic belt. We present detrital zircon U-Pb dating, trace element and in situ Lu-Hf isotope data for the Middle Triassic Leikoupo Formation and the Late Triassic Xujiahe Formation samples from the eastern Sichuan Basin, South China. The detrital zircon U-Pb ages of the Leikoupo Formation show seven age clusters of 280–242, 350–300, 500–400, 1000–800, 2000–1750, 2100–2000 and 2600–2400 Ma, while those of the Xujiahe Formation show five age clusters of 300–200, 500–350, 1050–950, 2000–1750 and 2600–2400 Ma. Combined with published paleocurrent and paleogeographic data, the sediments of the Leikoupo Formation are interpreted to be sourced from the North China Craton, Yangtze Craton and North Qinling orogenic belt, and the potential main source regions of the Xujiahe Formation included the South and North Qinling orogenic belts. Provenance analysis indicates that the North Qinling orogenic belt was in inherited uplift and coeval denudation in the Middle Triassic. The proportion of the detritus formed in the South Qinling orogenic belt increases gradually from the Leikoupo to Xujiahe formations. This significant provenance change indicates that rapid tectonic uplift and extensive denudation of the South Qinling orogenic belt occurred in the early Late Triassic, which is related to the collision between the North China and South China cratons during the Triassic.
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2025,99(2):441-458, DOI: 10.1111/1755-6724.15280
Abstract:
Large-scale Cenozoic alkali-rich magmatic rocks are exposed at the eastern margin of Tibet due to the interaction between the Indian and Eurasian plates. However, their petrogenesis and associated geodynamic processes remain poorly understood. We analyzed the Xifanping porphyries in the Sanjiang orogenic belt to provide new insights. Our study shows a successive assembly of porphyry intrusions during three magmatic episodes. The magnitude and duration of the magmatic activities diminished sequentially, and mineralization occurred during the intermediate phase. Geochemically, the Xifangping porphyries display an adakitic affinity. According to zircon Hf isotope data, we propose that these porphyries originated from the partial melting of the thickened mafic lower crust beneath the western Yangtze Craton in response to lithospheric extension and asthenospheric upwelling. Analogous to the coeval alkali-rich porphyries in western Yunnan, the petrogenetic model of the Xifanping porphyries indicates regional north–south and east–west fractures caused by the clockwise rotation of the continental lithosphere and the Jinshajiang–Red River strike-slip during the post-collision phase of the India–Eurasia collision. In this context, we argue that the collision in eastern Tibet may have extended eastward to southwestern Sichuan during the post-collision period, persisting until approximately 30 Ma.
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LIU Yu,JIANG Biao,WU Liwen,ZUO Yushan,LIU Zhao,LIU Haitao
2025,99(2):459-472, DOI: 10.1111/1755-6724.15215
Abstract:
The Shuangjianzishan deposit is a typical magmatic-hydrothermal deposit located in the southern Great Xing'an Range. Recent investigations have identified significant copper and tin mineralization at depth within the Shuangjianzishan deposit; however, the coupling relationship between magmatic emplacement and mineralization processes remains debated. This study presents whole-rock geochemistry, zircon LA-ICP-MS U-Pb dating, and zircon Hf isotope analyses of granite from the northern Shuangjianzishan deposit. The analysis results indicate the granite crystallized between 252.3 and 257.9 Ma, corresponding to Late Permian magmatic activity. The granite displays εHf(t) = 5.95–14.87, and tDM2 = 333–900 Ma. Geochemically, the granite is rich in Si and Al, with high K, classified as a calc-alkaline, weakly peraluminous rock. LREEs are enriched, while HREEs are depleted, and a slight negative Eu anomaly, all of which are consistent with A-type granite characteristics. The Hercynian granite in the Shuangjianzishan deposit formed during the latter or post-collisional stages of the collision orogeny following the closure of the Paleo-Asian Ocean in the late Paleozoic era. The material source indicates a mixed origin, involving both crust and mantle contributions. The granite is also enriched in Cu, Pb, and Zn, suggesting its potential role as an ore-forming material source for the Shuangjianzishan deposit. This study proposes a potential link between Hercynian magmatism and mineralization at the Shuangjianzishan deposit for the first time, suggesting that multistage metallogenesis may be a response to successive magmatic events from Hercynian to Yanshanian periods in the mining area.
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LUO Xinyu,LIU Biao,KONG Hua,JIANG Hua,WU Qianhong,YANG Jiehua,Safiyanu Muhammad ELATIKPO
2025,99(2):473-498, DOI: 10.1111/1755-6724.15286
Abstract:
The Late Cretaceous Jiepailing granitoids, located at the central Nanling Range in South China, are closely associated with significant Sn-Li-Be-F polymetallic metallogeny. The Jiepailing granitoids mainly consist of granitic porphyry and zinnwaldite granite. The two granitoids have an A-type affinity, showing elevated Rb/Sr ratios and significant depletions in Ba, Sr and P. Integrated zircon and monazite U-Pb dating results suggest that granitic porphyry and zinnwaldite granite were emplaced at ~89 Ma and ~94 Ma, respectively. The low Ce4+/Ce3+ ratios of the Jiepailing granitoids, together with significant negative Eu anomalies of the zircons, indicate that their formation occurred under conditions of reduced oxygen fugacity. Through the analysis of zircon Hf-O and whole-rock Nd isotopes, it has been determined that both stages of the Jiepailing granitoids originated in the lower-middle Mesoproterozoic crustal basement [εNd(t) = ?5.33 to ?4.96, tCDM(Nd) = 1289–1234 Ma, εHf(t) = ?4.13 to +2.22, tCDM(Hf) = 1418–1015 Ma and δ18OZrc = 6.33‰–7.72‰], with the involvement of mantle-derived materials. Both granitic porphyry and zinnwaldite granite exhibit elevated concentrations of fluorine (F), with the positive correlation between F and Sn emphasizing the crucial role of high F sources in tin mineralization. Drawing upon the study of the Late Cretaceous magma systems in southern Hunan and through comparison with the mineralized granites observed in coastal regions during the Late Cretaceous, a genetic model for the mineralized granites in the Nanling region is developed. When the Paleo-Pacific Plate retreated to the coastal region, the continental crust in southern China underwent extensional thinning and asthenospheric upwelling due to gravitational collapse. Such processes resulted in the partial melting of the middle–lower crustal metamorphic sedimentary basement and the subsequent formation of F-rich granitic magmas, related to tin mineralization.
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2025,99(2):499-521, DOI: 10.1111/1755-6724.15291
Abstract:
Controversy is ongoing regarding the relationship between ore formation and the structural evolution of the Hadamengou gold deposit. To address this issue, we conducted a comprehensive investigation of mineralization-related structures, geochronology and Fe isotopes. From the perspective of spatial evolution, hydrothermal fluids originating from the Shadegai and Xishadegai plutons have extracted accumulated ore-forming elements from the Wulashan Group (Ar2WL) and then evolved, initiating at Exploration Line 11 and migrating eastwards and westwards along the EW-trending thrust fault system to form orebodies. From the temporal evolution standpoint, the Wulashan Group (Ar2WL) experienced diagenesis (2591.00 Ma to 2204.00 Ma) and metamorphism (2074.00 Ma to 1625.00 Ma) from late Neoarchean to early Paleoproterozoic, when ore-forming materials were initially accumulated; in the early Paleozoic (440.71 Ma to 425.00 Ma), the collision led to the formation of early-stage EW-trending imbricated thrust faults, which established a fundamental structural framework for the orefield and further accumulated ore-forming materials; from the late Paleozoic to the Mesozoic, multiple subsequent episodes of regional tectonic-magmatic-hydrothermal events have superimposed, modified and reactivated the thrust fault system. Notably, the Triassic period, particularly between 245.00 Ma and 217.90 Ma, is considered to be a primary ore-forming stage. In summary, the intricate relationship between ore-formation and structural evolution has been fundamentally elucidated.
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WANG Xuhui,LANG Xinghai,WU Changyi,DENG Yulin,Robert MORITZ
2025,99(2):522-531, DOI: 10.1111/1755-6724.15283
Abstract:
The key factor that controls the genesis of porphyry Cu deposits (PCDs) in collisional orogens remains a debated topic. This study employs whole-rock La/Yb proxies to quantitatively constrain the spatial and temporal variations in crustal thickness of the South Armenian–Iranian magmatic belt (SAIMB) within the Zagros orogen (central Tethys region) since the Eocene. Our results show that rapid crustal thickening occurred first in the NW section of the SAIMB at ~35 Ma, then propagated southeastward into the central and SE sections at ~25 Ma and 20 Ma, respectively, indicating that the Arabia–Eurasia collision was diachronous. The formation of the large and giant collision-related PCDs in the SAIMB might have been controlled by the collision process because they developed first in the NW section of the SAIMB and subsequently propagated southeastward into the central and SE sections. More importantly, crustal thickness mapping shows that the PCDs are preferentially developed in the thickened crust areas (>50 km). Our findings propose that thickened crust is critical for the formation of the PCDs in collisional orogens by promoting Fe2+-rich minerals as a fractionating phase, driving magmatic auto-oxidation and releasing Cu into the magmas. The Cu is then partitioned into magmatic fluids, sustaining the porphyry systems. Furthermore, our research highlights that the thickened crust hosting PCDs was characterized by a previously thinner crust (<40 km), where magmas had low oxygen fugacity due to the absence of the auto-oxidation process. Consequently, chalcophile elements (e.g., Cu) efficiently separated from the melt through sulfide segregation, forming large Cu-bearing lower-crustal cumulates. These cumulates can be mobilized with an increase in oxygen fugacity, incorporating into subsequent porphyry mineralization. We thus propose that the crustal thickness evolution over time controls the formation of the PCDs in collisional orogens. There are two essential stages in the collision-related PCDs formation: the first is high-flux magmatism in the thin crustal setting (<40 km), leading to metal-fertilized lower crust through sulfide segregation, and the second is the intracrustal auto-oxidation during crustal thickening (>50 km) which facilitates pre-enriched sulfides in the lower crust to re-dissolve, releasing Cu into the magmas.
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2025,99(2):532-552, DOI: 10.1111/1755-6724.15281
Abstract:
Although previous researchers have attempted to decipher ore genesis and mineralization in the Erdaokan Ag-Pb-Zn deposit, some uncertainties regarding the mineralization process and evolution of both ore-forming fluids and magnetite types still need to be addressed. In this study, we obtained new EPMA, LA-ICP-MS, and in situ Fe isotope data from magnetite from the Erdaokan deposit, in order to better understand the mineralization mechanism and evolution of both magnetite and the ore-forming fluids. Our results identified seven types of magnetite at Erdaokan: disseminated magnetite (Mag1), coarse-grained magnetite (Mag2a), radial magnetite (Mag2b), fragmented fine-grained magnetite (Mag2c), vermicular gel magnetite (Mag3a1 and Mag3a2), colloidal magnetite (Mag3b) and dark gray magnetite (Mag4). All of the magnetite types were hydrothermal in origin and generally low in Ti (<400 ppm) and Ni (<800 ppm), while being enriched in light Fe isotopes (δ56Fe ranging from ?1.54‰ to ?0.06‰). However, they exhibit different geochemical signatures and are thus classified into high-manganese magnetite (Mag1, MnO > 5 wt%), low-silicon magnetite (Mag2a-c, SiO2 < 1 wt%), high-silicon magnetite (Mag3a-b, SiO2 from 1 to 7 wt%) and high-silicon-manganese magnetite (Mag4, SiO2 > 1 wt%, MnO > 0.2 wt% ), each being formed within distinct hydrothermal environments. Based on mineralogy, elemental geochemistry, Fe isotopes, temperature trends, TMg-mag and (Ti + V) vs. (Al + Mn) diagrams, we propose that the Erdaokan Ag-Pb-Zn deposit underwent multi-stage mineralization, which can be broken down into four stages and nine sub-stages. Mag1, Mag2a-c, Mag3a-b and Mag4 were formed during the first sub-stage of each of the four stages, respectively. Additionally, fluid mixing, cooling and depressurization boiling were identified as the main mechanisms for mineral precipitation. The enrichment of Ag was significantly enhanced by the superposition of multi-stage ore-forming hydrothermal fluids in the Erdaokan Ag-Pb-Zn deposit.
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Jyoti Sankar SATAPATHY,Sahendra SINGH,Prabodha Ranjan SAHOO
2025,99(2):553-567, DOI: 10.1111/1755-6724.15289
Abstract:
Emerald mineralization from the Bahutiya and Gurabanda areas of Jharkhand in the eastern part of India is a recent discovery. In this deposit, emerald mineralization occurs along the contact zone between pegmatite and epidiorite-hornblende schist of the Dhanjori Group (2.1–2.9 Ga). Host rock petrographic characteristics, along with the spatial distribution of the emerald, suggest a metasomatic origin for the emerald mineralization in the study area. The well-developed emerald crystals are found along the S2 schistosity plane, suggesting lithological and structural control on the mineralization. Electron microprobe data of the emerald indicates that the green hue is primarily due to the variable chromium content and Be could have been derived from the soda-granite of the Singhbhum Shear Zone. The average Cr2O3 and Cr concentration in the emerald is 0.038 wt% and 0.003 apfu, respectively. The ternary diagrams FeO–MgO–Cr2O3 and FeO–Cr2O3–V2O5 are plotted and superimposed on global emerald data, compiled from the literature, which shows the similarity of this deposit to other emerald deposits of the world. From the present study, it is inferred that the emerald deposits of Bahutiya and Gurabanda, Jharkhand, belong to the Type-IA category.
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2025,99(2):568-581, DOI: 10.1111/1755-6724.15285
Abstract:
Recent exploration has highlighted the critical role of strike-slip faults in shaping ultra-deep carbonate reservoirs in the Tarim Basin. This study integrates satellite imagery, UAV photogrammetry, outcrop surveys and microscopic analysis to investigate the architecture of these faults and their impact on reservoir petrophysical properties. The strike-slip faults exhibit cores consisting of calcite bands, fault breccias and fractures, while the damage zones are predominantly fractured. Thicker fault cores and fault zones are associated with more extensive reservoir development. Individual strike-slip fault zones are primarily characterized by two sets of fractures intersecting the fault at small angles. When two fault systems interact, the dominant pattern is two sets of fractures intersecting the main fault at small angles and one set at larger angles, facilitating the formation of large-scale reservoirs. We propose a model for the fault core, which primarily consists of a calcite band and fault breccias. These breccias are composed of original host rock, calcite cement and quartz, which exhibit poor physical properties, while fractures and vugs show favorable reservoir characteristics. This model offers valuable insights into the development of fault-controlled reservoirs, particularly in the Tarim Basin.
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HE Lijuan,YU Qiang,REN Zhanli,LI Rongxi,LEI Xianghe,SUN Xianyao,YANG Qike,WANG Tianzi,YUAN Ruize
2025,99(2):582-597, DOI: 10.1111/1755-6724.15278
Abstract:
The present-day pressure pattern is the ultimate result of the evolution of paleo-pressure, so understanding the variation of stress throughout geological history is of great significance for oil and gas accumulation. In this study, the fission track method was used to reconstruct the cooling history of sandstone samples from the Yanchang Fm. in the central–eastern Ordos Basin and the cause of the low-pressure anomaly in the Yanchang Fm. was analyzed. The max. burial depth pressure was reconstructed and the pressure evolution of the formation in the Futan 1 well was simulated, using Petromod 1D. The fission track data and Petromod 1D simulation results indicate that the Yanchang Fm. reached its max. burial depth and experienced a high paleo-pressure of 30.92 MPa at around 100 Ma. Since the Late Cretaceous, the formation pressure evolution in the study area can be divided into two stages. From 100 to 20 Ma, the formation slowly uplifted, with the pressure gradually decreasing. Since the Miocene (about 20 Ma), the pressure rapidly decreased to the current pressure of approximately 6.92 MPa. Based on the above research results, the influence of pore rebound and temperature decrease on formation pressure was quantitatively calculated. The results show that during the first stage, the pressure reduction caused by pore rebound and cooling was 3.86 MPa and 3.49 MPa, respectively, with a decrease of about 12.48% and 11.28%. During the second stage, the pressure reduction caused by pore rebound and cooling was 6.32 MPa and 9.60 MPa, respectively, with a decrease of about 20.43% and 31.04%. The formation of low pressure in the Yanchang Fm. in the central and eastern basin is mainly controlled by pore rebound and temperature reduction, caused by erosion after stratigraphic uplift. The decrease in temperature plays a decisive role in determining the formation process of the low-pressure oil reservoir.
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2025,99(2):598-610, DOI: 10.1111/1755-6724.15276
Abstract:
The SiO2'–CaO/(CaO + K2O) (S'CK) diagram is an empirically derived major element-based equivalent to the modal IUGS alkali feldspar–quartz–plagioclase classification scheme for granitoids. It employs the content of SiO2 and CaO/(CaO + K2O) ratio to approximate the IUGS classification diagram and a normative-based Q'–ANOR plot. Four trends have been superimposed onto the SiO2'–CaO/(CaO + K2O) diagram based on published datasets from the Peninsular Ranges (calcic: C), Tuolumne (calc–alkalic: CA), Sherman (alkali–calcic: AC), and Bjerkreim-Sokndal (alkalic: A) batholiths, which were employed to constrain the positions of the C–CA, CA–AC and AC–A suite boundaries on the SiO2 versus (Na2O + K2O – CaO) (or modified alkali–lime index, MALI) granitic classification diagram. A merit of the SiO2'–CaO/(CaO + K2O) plot is identifying rock types comprising a suite and their relative abundances. The distinguished projections of five typical granitoid assemblages, which are summarized by Bonin et al. (2020), demonstrate the ability of SiO2'–CaO/(CaO + K2O) diagram to decipher their petrogenesis. The SiO2' –CaO/(CaO + K2O) plots for the plutonic suites of 'known' tectonic settings can reveal their evolution paths and the lithological statistics. Accordingly, it is suggested that the SiO2'–CaO/(CaO + K2O) plot can distinguish the tectonic environments of plutonic suits by comparing the plutonic suites or batholiths of 'unknown' tectonic context to the published datasets from granitoid suites formed within 'known' tectonic settings. The modified SiO2'–CaO/(CaO + K2O) diagram links the bulk chemical composition of granitoid suites to the likely source, magmatic evolution, and tectonic setting; thus, it may be a useful tectono-magmatic classification scheme for granitoid suites.
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YUAN Lingling,CHAI Peng,HOU Zengqian,QUAN Haihui,SU Chongbin
2025,99(2):611-624, DOI: 10.1111/1755-6724.15277
Abstract:
Numerous intermediate to felsic igneous rocks are present in both subduction and collisional orogens. However, porphyry copper deposits (PCDs) are comparatively rare. The underlying factors that differentiate fertile magmas, which give rise to PCDs, from barren magmas in a specific geological setting are not well understood. In this study, three supervised machine learning algorithms: random forest (RF), logistic regression (LR) and support vector machine (SVM) were employed to classify metallogenic fertility in southeastern Tibet, Sanjiang orogenic belt, based on whole-rock trace element and Sr-Nd isotopic ratios. The performance of the RF model is better than LR and SVM models. Feature importance analysis of the models reveals that the concentration of Y, Eu, and Th, along with Sr-Nd isotope compositions are crucial variables in distinguishing fertile and barren samples. However, when the optimized models were applied to predict the datasets of Miocene Gangdese porphyry copper belt and Jurassic Gangdese arc representing collision and subduction settings respectively, a marked decline in metrics occurred in all three models, particularly on the subduction dataset. This substantial decrease indicates the compositional characteristics of intrusions across different tectonic settings could be diverse in a multidimensional space, highlighting the complex interplay of geological factors influencing PCD’s formation.
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2025,99(2):626-626, DOI:
Abstract:
2025年第99卷第2期
2025年第99卷第2期
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青藏高原东北缘祁连–海原断裂带中段金强河断裂晚第四纪滑动行为
梁淑敏, 郑文俊, 陈干, 张培震, 张冬丽, 毕海芸, 杨雪, 张逸鹏, 段磊, 卢本添
Abstract:
祁连–海原断裂带控制着青藏高原东北缘地区的强震活动。在其中段的金强河断裂是天祝地震空区一条关键的活动断裂,但目前对该断裂的滑动行为认识不足。本文针对沿金强河断裂的水平位移分布,利用WorldView-2立体像对和无人机摄影测量数据,提取断裂沿线高精度的DEM数据,并进行精细的构造地貌解译和水平位错测量。通过断错地貌标志的测量,得到135个位错量和8个位错丛集。同时,利用放射性碳测年方法构建4个典型点断错河流阶地的地貌单元年龄序列,从而通过位错与年龄的关系将位错丛集和地貌单元年龄序列关联起来,并获得金强河断裂全新世的滑动速率在 ~4–12 ka期间为4.8–5.6 mm/a ,在 ~4 ka以来为2.9–4.7 mm/a。最近的三次地震事件的复发间隔约为1000年,形成了一个地震活跃期,揭示着近1500年来缺乏破裂记录的金强河断裂可能具有较高的地震危险性。
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南阿尔金早古生代构造演化:来自茫崖花岗质岩石地球化学、锆石U-Pb和Lu-Hf同位素的证据
徐楠, 吴才来, 刘和武, 宋帅兵, 张贵生, 郑坤, 高栋
Abstract:
南阿尔金造山带是中国西南典型的俯冲造山带,由南阿尔金蛇绿混杂岩带和南阿尔金陆块组成,位于柴达木板块北侧。造山带出露大量早古生代花岗质岩石,但是这些岩石的成因及构造环境尚未查明。本文对茫崖花岗质岩石进行岩石学和地球化学研究,确定岩浆活动的期次,并深入了解南阿尔金造山带的构造演化过程。茫崖花岗质岩浆活动可以划分为三期:494-458Ma,450-436Ma和416-404Ma。根据这些岩石的成岩构造环境,我们认为第一期岩浆活动与南阿尔金洋的北向俯冲有关,形成了大量高价钙碱性、I型花岗质岩石。南阿尔金洋闭合后,柴达木板块开始向南阿尔金陆块碰撞,行了了一系列高价钙碱性、I型花岗岩。第三期岩浆活动形成了大量的造山后A-型花岗岩。
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超微量(80nanomole)硫化物硫酸盐硫同位素的EA-IRMS测试
Abstract:
常规EA-IRMS进行硫同位素测试时需硫量大于2 μmol,这限制了该技术在测试含硫量低的样品时的使用。如此大的需硫量是因为He载气携带样品气体在经过元素分析仪(EA)时的流速为~100 mL/min,而气体同位素质谱仪仅允许气体以低流速进入,所以99.7%的混合气体会通过连续流接口排出,以保证混合气体以~0.3 mL/min的流速通过连续流接口。因此,大部分的样品气体会被浪费,样品的利用率仅有0.3%。在本研究中,我们将自主研发的冷冻富集、分离与纯化系统与EA-IRMS联用测试了六种标准物质的硫同位素,并检测该系统的表现。实验结果表明,使用本研究中改进的方法进行硫化物和硫酸盐标准物质的硫同位素测试,得到的硫同位素结果与常规方法一致,即需硫量仅80 nmol即可得到硫同位素测试结果精度 ±0.24‰–±0.76‰ (1σ),与使用吸附柱进行硫同位素测试的方法获得的精度相似。所以,改进后的EA-IRMS可以实现超微量硫化物、硫酸盐的硫同位素测试。此外,本方法也可应用至需样量低至100 nmol的碳、氮和氧同位素分析测试工作中。
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粤北早古生代强过铝质花岗岩及其共生岩石的岩石成因及对广西运动的指示意义:来自元素和Sr-Nd-Hf同位素的制约
Abstract:
本文系统报道了粤北地区早古生代强过铝质花岗岩及其共生岩石的锆石U-Pb年代学、主、微量元素及Sr-Nd-Hf同位素组成,探讨其源区特征、岩石成因及构造意义。青州花岗闪长岩为弱-强过铝质,A/CNK= 1.05–1.96。它们具有相对高的初始Sr同位素组成ISr= 0.7087– 0.7148和低的εNd(t)值(-11.2 – -10.1),以及变化的εHf(t)值-13.4– +4.81。与之不同,大帽山花岗闪长岩为准铝质(A/CNK= 0.79– 0.94),ISr= 0.7083– 0.7110, εNd(t)= -7.92– -5.28和εHf(t)= -8.69– -2.06。高寿石英闪长岩为准铝-强过铝质(0.87– 1.24),ISr值和εNd(t)值分别为0.7104– 0.7111和-9.64– -8.63。元素和Sr-Nd-Hf同位素组成结果显示,青州、大帽山和高寿花岗质侵入岩主要分别源自变杂砂岩、英安质岩和角闪石岩的部分熔融。结合前人的研究成果,这些强过铝质花岗岩形成于同造山环境。本文尝试提出一种关于华南早古生代花岗岩的岩石成因及区域地壳重组的新思路。而广西运动动力机制的揭示需要更加广阔的视野和更加丰富的地质证据。
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Birendra P. Singh, Kapesa Lokho, Naval Kishore, Nancy Virmani
2014,88(2):380-393, DOI:
Abstract:
A new locality bearing ichnofossils of the Cruziana Assemblage Zone-III from the Mussoorie syncline, Lesser Himalaya, is located in rocks of Member-B of the Dhaulagiri Formation, Tal Group, exposed along the Maldewta-Chhimoli fresh road cut section. The site yielded ichnofossils Bergaueria perata, Cochlichnus anguineus, ?Diplocraterion isp., Dimorphichnus obliquus, diplichnitiform Cruziana bonariensis, Diplichnites gouldi, Glockeria isp., Helminthopsis isp., Monomorphichnus lineatus, Phycodes palmatum, Palaeophycus striatus, Planolites beverleyensis, Planolites montanus, Treptichnus cf. T. pedum, scratch marks and an undetermined worm impression. An Early Cambrian age (Cambrian Series 2) is assigned to the ichnofossil-bearing strata based on the stratigraphic position between the Drepanuroides and Palaeoolenus trilobite zones. A revised Cambrian ichnofossil zonation is presented for the Tal Group of the Mussoorie syncline. Together with their occurrence on rippled surfaces, and the lateral displacement of some trackways (due to current action), a sub-aqueous shallow-marine depositional setting is proposed for the rocks of Member-B.
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ZHU Song, WU Zhenhan, ZHAO Xitao, LI Jianping, WANG Hua
2012,86(1):266-283, DOI:
Abstract:
Many moraines formed between Daduka and Chibai in the Tsangpo River valley since Middle Pleistocene. A prominent set of lacustrine and alluvial terraces on the valley margin along both the Tsangpo and Nyang Rivers formed during Quaternary glacial epoch demonstrate lakes were created by damming of the river. Research was conducted on the geological environment, contained sediments, spatial distribution, timing, and formation and destruction of these paleolakes. The lacustrine sediments 14C (10537±268 aBP at Linzhi Brick and Tile Factory, 22510±580 aBP and 13925±204 aBP at Bengga, 21096±1466 aBP at Yusong) and a series of ESR (electron spin resonance) ages at Linzhi town and previous data by other experts, paleolakes persisted for 691~505 kaBP middle Pleistocene ice age, 75–40 kaBP the early stage of last glacier, 27–8 kaBP Last Glacier Maximum (LGM), existence time of lakes gradually shorten represents glacial scale and dam moraine supply potential gradually cut down, paleolakes and dam scale also gradually diminished. This article calculated the average lacustrine sedimentary rate of Gega paleolake in LGM was 12.5 mm/a, demonstrates Mount Namjagbarwa uplifted strongly at the same time, the sedimentary rate of Gega paleolake is more larger than that of enclosed lakes of plateau inland shows the climatic variation of Mount Namjagbarwa is more larger and plateau margin uplifted more quicker than plateau inland. This article analyzed formation and decay cause about the Zelunglung glacier on the west flank of Mount Namjagbarwa got into the Tsangpo River valley and blocked it for tectonic and climatic factors. There is a site of blocking the valley from Gega to Chibai. This article according to moraines and lacustrine sediments yielded paleolakes scale: the lowest lake base altitude 2850 m, the highest lake surface altitude 3585 m, 3240 m and 3180 m, area 2885 km2, 820 km2 and 810 km2, lake maximum depth of 735 m, 390 m and 330 m. We disclose the reason that previous experts discovered there were different age moraines dividing line of altitude 3180 m at the entrance of the Tsangpo Grand Canyon is dammed lake erosive decay under altitude 3180 m moraines in the last glacier era covering moraines in the early ice age of late Pleistocene, top 3180 m in the last glacier moraine remained because ancient dammed lakes didn’t erode it under 3180 m moraines in the early ice age of late Pleistocene exposed. The reason of the top elevation 3585 m moraines in the middle Pleistocene ice age likes that of altitude 3180 m. There were three times dammed lakes by glacier blocking the Tsangpo River during Quaternary glacial period. During other glacial and interglacial period the Zelunglung glacier often extended the valley but moraine supplemental speed of the dam was smaller than that of fluvial erosion and moraine movement, dam quickly disappeared and didn’t form stable lake.
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WANG Runfu, XU Shichao, WU Xiaochun, LI Chun, WANG Suozhu
2013,87(5):1185-1197, DOI:
Abstract:
Shansisuchus shansisuchus Young, 1964 was restudied on the basis of a new specimen. Some anatomical features that were either briefly or not described at all in the original study were detailed. The new specimen not only provides further information on the skull anatomy and the vertebral column but also expands the range of the geographical distribution of the taxon. With new information, the diagnosis of S. shansisuchus was emended and its phylogenetic relationships were further analyzed. S. shansisuchus differs from other archosauriforms primarily in the presence of a large subnarial fenestra anterior to the antorbital fenestra, tongue-in-groove articulations between the ascending process of the premaxilla and nasal and between the premaxilla and maxilla, a tall and posterodorsally directed ascending process of the maxilla, a knee-shaped process of the postorbital projecting into the orbit, a broad descending process of squamosal distally well forked and a large, deeply bow-shaped intercentrum tightly anchoring/capping the sharp ventral edges of two neighboring centra together in cervical and at least first eight dorsal vertebrae. With additional information derived from the new specimen, the phylogenetic relationships of S. shansisuchus were reanalyzed; it is closely related to Erythrosuchus-Vjushkovia clade.
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CHEN Lan1, 2, 3, * , YI Haisheng4, 5, TSAI Louis Loung-Yie2, XU Guiwen1, DA Xuejuan1, LIN Andrew Tien-Shun3
2013,87(2):540-554, DOI:
Abstract:
The Biluo Co and Amdo 114 station, northern Tibet, cropping out the Early Toarcian and Middle-Late Tithonian (Jurassic) organic-rich black shales, have been a focus to petroleum geologists in discussing their oil-producing potential. This paper first reports the trace elements and rare earth elements to discuss the paleoenvironments, redox conditions and sedimentary mechanisms of those black shales. Both sections exhibit variation in trace element abundances with concentrations <0.1 ppm to 760 ppm, mostly enriched in V, Cr, Ni, Cu, Zn, Mo, Ba and U. Element ratios of Ni/Co, V/Cr, U/Th and V/(V+Ni) plus U were used to identify redox conditions. The shale-normalized rare earth element (REE) patterns are characterized by the flat-shale type with instable Ce anomalies and very weekly positive Eu anomalies. Positive Ceanom values are significant with values varying between –0.064 and 0.029 in Biluo Co, which may be interpreted as release of REE and input of riverine terrestrial matter with rich Ce (resulting in pH change) during the anoxic conditions. In the middle parts of Amdo 114 station, distinct negative Ceanom values are observed (?0.238 to ?0.111) and associated surface water warming were interpreted as being related to a major sea level rise. In contrast, the formation of the black shales in the lower and upper part of the studied succession took place during a cooler (Ceanom values >–0.10), lower surface water productivity, and lower sea-level stage. Thus, we emphasize the role of different factors that control the formation of local and regional black shales. The most important factors are sea-level fluctuations and increasing productivity.
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2014,88(1):260-275, DOI:
Abstract:
This paper reviews the current progress and problems in the study of microbialites and microbial carbonates. Microbialites and microbial carbonates, formed during growth of microbes by their calcification and binding of detrital sediment, have recently become one of the most popular geological topics. They occur throughout the entire geological history, and bear important theoretical and economic significances due to their complex structures and formative processes. Microbialites are in place benthic microbial buildups, whereas microbial carbonates can be classified into two categories: stabilized microbial carbonates (i.e., carbonate microbialites, such as stromatolites and thrombolites) and mobilized microbial carbonates (i.e., microbial carbonate grains, such as oncoids and microbial lumps). Various texture, structures, and morphologies of microbialites and microbial carbonates hamper the systematic description and classification. Moreover, complex calcification pathways and diagenetic modifications further obscure the origin of some microbialites and microbial carbonates. Recent findings of abundant sponge spicules in previously identified “microbialites” challenge the traditional views about the origins of these “microbialites” and their implications to reef evolution. Microbialites and microbial carbonates did not always flourish in the aftermath of extinction events, which, together with other evidences, suggests that they are affected not only by metazoans but also by other geological factors. Their growth, development, and demise are also closely related to sea-level changes, due to their dependence on water depth, clarity, nutrient, and sunlight. Detailed studies on microbialites and microbial carbonates throughout geological history would certainly help understand causes and effects of major geological events as well as the co-evolution of life and environment.
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SHEN Caizhi, Lü Junchang, LIU Sizhao, Martin KUNDRáT, Stephen L. BRUSATTE, GAO Hailong
2017,91(3):763-780, DOI:
Abstract:
A new troodontid dinosaur, Daliansaurus liaoningensis gen. et sp. nov., is erected based on a nearly complete specimen from the Lower Cretaceous Yixian Formation of Beipiao City, Liaoning Province, China. This well preserved skeleton provides important new details of the anatomy for Liaoning troodontids, and gives new insight into their phylogenetic relationships and evolution. Daliansaurus is distinguished from other troodontids by an enlarged ungual on pedal digit IV, which is approximately the same size as the sickle-shaped second ungual, and is differentiated from other Liaoning troodontids by a number of characters of the skull, manus, pelvis, and hindlimb. A phylogenetic analysis recovers Daliansaurus within a subclade of Liaoning troodontids that also includes Sinovenator, Sinusonasus, and Mei. We erect a name for this group—Sinovenatorinae—and argue that it reflects a localized radiation of small-bodied troodontids in the Early Cretaceous of eastern Asia, similar to previously recognized radiations of Liaoning dromaeosaurids and avialans. As more Liaoning theropods are discovered, it is becoming apparent that small, feathered paravians were particularly diverse during the Early Cretaceous, and future work is needed to clarify how this diversity arose, which species coexisted, and how these numerous species partitioned niches.
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2014,88(z2):597-598, DOI:
Abstract:
Please refer to the attachment(s) for more details
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DU Chunguo, WANG Jianjun, ZHANG Jun, WANG Ping, XUE Mei, ZHOU Huayao
2014,88(3):865-877, DOI:
Abstract:
On the basis of field observations, microscopic thin-sections and laboratory data analysis of ten faults in Xuanhan County area, northeastern Sichuan Basin, central China, the internal and megascopic structures and tectonite development characteristics are mainly controlled by the geomechanical quality in brittle formation of the Changxing-Feixianguan Formation. The fluid transportation performance difference between the faults formed by different geomechanics or different structural parts of the same fault are controlled by the megascopic structure and tectonite development characteristics. For instance, the extension fault structure consists of a tectonite breccia zone and an extension fracture zone. Good fluid transportation performance zones are the extension fracture zone adjacent to the tectonite breccia zone and the breccia zone formed at the early evolutionary stage. The typical compression fault structure consists of a boulder-clay zone or zones of grinding gravel rock, compression foliation, tectonite lens, and dense fracture development. The dense fracture development zone is the best fluid transporting area at a certain scale of the compression fault, and then the lens, grinding gravel rock zone and compression foliation zones are the worst areas for hydrocarbon migration. The typical tensor-shear fault with a certain scale can be divided into boulder-clay or grinding gravel rock zones of the fault, as well as a pinnate fractures zone and a derivative fractures zone. The grinding gravel rock zone is the worst one for fluid transportation. Because of the fracture mesh connectivity and better penetration ability, the pinnate fractures zone provides the dominant pathway for hydrocarbon vertical migration along the tensor-shear fault.
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MA Shengming, ZHU Lixin, LIU Chongmin, XI Mingjie, TANG Shixin
2013,87(3):843-857, DOI:
Abstract:
This paper discusses the enrichment and depletion regularities for porphyry copper-molybdenum ore deposits in different regions and varied deposit genetic types in the same area, taking three porphyry copper-molybdenum ore deposits (i.e., the Chengmenshan in Jiangxi, Wunugetushan in Inner Mongolia, Baishantang in Gansu) and two copper deposits in Gansu Province (the Huitongshan skarn deposit and Gongpoquan composite deposit) as case studies. The results show that porphyry Cu-Mo deposits or skarn copper deposits include both enrichment of the ore-forming elements and associated elements, and depletion of some lithophile dispersed elements, rare earth elements (REE) and some major elements. And the depleted elements vary with deposits, having generality and their own features. On a deposit scale, the positive anomalies of enriched elements and negative anomalies of depleted elements follow in a sequence to comprise regular anomaly models of spatial structures. The exploration in the Tongchang deposit in Jiangxi and Huitongshan deposit in Gansu suggests that anomaly models play a key role in the identification of mineral occurrences and deposits compared to one single enriched element anomaly. And the anomaly models exert a critical effect on the optimization of prospecting targets and their potential evaluation.
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2010,84(2):241-246, DOI:
Abstract:
A new boreopterid pterosaur: Zhenyuanopterus longirostris gen. et sp. nov. from the Yixian Formation of western Liaoning is erected, based on the complete skeleton with a skull and lower jaws preserved. It is characterized by: a large boreopterid pterosaur with a high number of teeth, where the anterior teeth are much larger than posterior ones; the length of the dorsal + sacral vertebrae is nearly half the length of the skull; ratio of the length of the humerus to metacarpal IV is approximately 91% and the, humerus, femur and third wing phalanx are all equal in length and the feet are specially small. It represents the largest boroepterid pterosaur discovered from western Liaoning and its surrounding areas so far
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WANG Sufen, ZHANG Tingshan, ZHOU Jixian, HU Yu
2017,91(1):320-340, DOI:
Abstract:
The distribution characteristics of the oil-water contact are the basis for the reservoir exploration and development and reserves evaluation. The reservoir with a tilted oil-water contact has a unique formation mechanism, and the understanding of its distribution and formation mechanism will directly affect the evaluations for the reservoir type, well deployment, selection of well pattern and type, determination of test section, and reserves evaluation. Based on the analysis of reservoir characteristics, petrophysical properties and geological structure in 40 reservoirs worldwide with tilted oil-water contacts, the progress of the research on the formation mechanisms of titled oil-water contacts is summarized in terms of the hydrodynamic conditions, reservoir heterogeneity, neotectonic movement and oil-gas exploitation. According to the formation mechanism of tilted oil-water contacts and the needs of exploration research, different aspects of research methods are summarized and classified, such as the calculation of equipotential surfaces for oil and water in the formation, analysis of formation pressure and analysis of reservoir physical properties and so on. Based upon statistical analysis, it is suggested that the degree of the inclination of the oil-water contact be divided based on the dip of oil-water contact (DipTOWC). The tilted oil-water contact is divided into three categories: large dip (DipTOWC≥55 m/km), medium dip (4 m/km≤DipTOWC<55 m/km), and small dip (DipTOWC<4 m/km). The classification and evaluation method can be combined with structure amplitude and reservoir property. The formation mechanism of domestic and international reservoirs with tilted oil-water contacts are summarized in this paper, which have important significance in guiding the exploration and development of the oilfield with tilted oil-water contacts, reserves evaluation, and well deployment.
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Mahboobeh JAMSHIDI BADR, Fariborz MASOUDI, Alan S. COLLINS, Ali SORBI
2012,86(1):48-64, DOI:
Abstract:
The Soursat metamorphic complex (SMC) in northwestern Iran is part of the Sanandaj–Sirjan metamorphic belt. The complex is composed of different metamorphic and plutonic rocks, but is dominated by metapelites composed of garnet, staurolite, kyanite, fibrolite, cordierite, and andalusite. Porphyroblasts in schists have the same fabric, and three stages of schistosity are present. The internal schistosity (Sn) inclusion trails are also offset by conjugate sets of extensional schistosity (Sn+1) and a second (Sn+2) that crenulates (Sn+1). Polyphase metamorphisms are present in the complex. Garnet, staurolite, kyanite, and fibrolite assemblage preserves conditions during the M1 metamorphic event. This assemblage yields a P–t estimate of 645±11°C and 6.5±0.5 kbar. Other samples of the central part of SMC contain cordierite and andalusite (M2) overgrowth that yields a P–t estimate of 532±33°C and 2.1±1.1 kbar.
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ZHENG Yadong, ZHANG Qing, HOU Quanlin
2015,89(4):1133-1152, DOI:
Abstract:
The essential difference in the formation of conjugate shear zones in brittle and ductile deformation is that the intersection angle between brittle conjugate faults in the contractional quadrants is acute (usually ~60°) whereas the angle between conjugate ductile shear zones is obtuse (usually 110°). The Mohr-Coulomb failure criterion, an experimentally validated empirical relationship, is commonly applied for interpreting the stress directions based on the orientation of the brittle shear fractures. However, the Mohr-Coulomb failure criterion fails to explain the formation of the low-angle normal fault, high-angle reverse fault, and the conjugate strike-slip fault with an obtuse angle in the σ1 direction. Although it is ten years since the Maximum-Effective-Moment (MEM) criterion was first proposed, and increasingly solid evidence in support of it has been obtained from both observed examples in nature and laboratory experiments, it is not yet a commonly accepted model to use to interpret these anti-Mohr-Coulomb features that are widely observed in the natural world. The deformational behavior of rock depends on its intrinsic mechanical properties and external factors such as applied stresses, strain rates, and temperature conditions related to crustal depths. The occurrence of conjugate shear features with obtuse angles of ~110° in the contractional direction on different scales and at different crustal levels are consistent with the prediction of the MEM criterion, therefore ~110° is a reliable indicator for deformation localization that occurred at medium-low strain rates at any crustal levels. Since the strain–rate is variable through time in nature, brittle, ductile, and plastic features may appear within the same rock.
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CHI Guoxiang1, *, CHU Haixia1, Ryan SCOTT1, CHOU I-Ming2
2014,88(4):1169-1182, DOI:
Abstract:
Raman peaks of various hydrates in the H2O-NaCl-CaCl2 system have been previously identified, but a quantitative relationship between the Raman peaks and XNaCl (i.e., NaCl/(NaCl+CaCl2)) has not been established, mainly due to the difficulty to freeze the solutions. This problem was solved by adding alumina powder to the solutions to facilitate nucleation of crystals. Cryogenic (-185oC) Raman spectroscopic studies of alumina-spiced solutions indicate that XNaCl is linearly correlated with the total peak area fraction of hydrohalite. Capsules of solutions made from silica capillary were prepared to simulate fluid inclusions. Most of these artificial fluid inclusions could not be totally frozen even at temperatures as low as -185oC, and the total peak area fraction of hydrohalite is not correlated linearly with XNaCl. However, the degree of deviation (DXNaCl) from the linear correlation established earlier is related to the amount of residual solution, which is reflected by the ratio (r) of the baseline “bump” area, resulting from the interstitial unfrozen brine near 3435 cm-1, and the total hydrate peak area between 3350 and 3600 cm-1. A linear correlation between DXNaCl and r is established to estimate XNaCl from cryogenic Raman spectroscopic analysis for fluid inclusions.
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LI Jianjun, Martin G. LOCKLEY, ZHANG Yuguang, HU Songmei, MATSUKAWA Masaki, BAI Zhiqiang
2012,86(1):1-10, DOI:
Abstract:
A large track site with multiple, well-preserved trackways of an Early Jurassic quadrupedal ornithischian dinosaur is the first report of Moyenisauripus-like trackways from Asia, herein named Shenmuichnus youngteilhardorum. The tracks occur in a clastic fluvial sequence in the Fuxian Formation in Shenmu County, Shaanxi Province, which is in the same general region as the discovery site of Sinoichnites,the first dinosaur track reported from China. Based on size and morphology, it is likely that Sinoichnites, which is now lost, also represents an ornithischian. The Shenmuichnus youngteilhardorum trackways show two modes of preservation: the first representing deeper tracks, with sediment rims, results in Deltapodus-like tracks, with indistinct pes digit traces and sub-circular manus traces, the second produces Moyenosauripus-like tracks, with clear tridactyl and pentadactyl digit traces in the pes and manus respectively. Thus the Shenmu trackways play a key role in resolving globally significant ichnotaxonomic problems surrounding the nomenclature of Sinoichnites, Moyenosauripus, Deltapodus and other named (Ravatichnus) and unnamed trackways from Asia, Africa and Europe. In addition they shed important light on the paleogeographical and paleoecological distribution of quadrupedal ornithischians in the Early Mesozoic. The track site has been the focus of a major excavation to transfer the trackways from their original remote location to the new Shenmu Museum, in Shenmu City. Other tracksites in the area which reveal Anomoepus, Grallator and the Deltapodus morphotype, together with Shenmuichnus and plant fossil evidence, suggest an Early Jurassic age for the tracksite.
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DU Jianjun, LI Dunpeng, WANG Yufang, MA Yinsheng
2017,91(1):76-92, DOI:
Abstract:
The Weihe Graben is not only an important Cenozoic fault basin in China but also a significant active seismic zone. The Huashan piedmont fault is an important active fault on the southeast side of the Weihe Graben and has been highly active since the Cenozoic. The well–known Great Huaxian County Earthquake of 1556 occurred on the Huashan piedmont fault. This earthquake, which claimed the lives of approximately 830000 people, is one of the few large earthquakes known to have occurred on a high–angle normal fault. The Huashan piedmont fault is a typical active normal fault that can be used to study tectonic activity and the associated hazards. In this study, the types and characteristics of late Quaternary deformation along this fault are discussed from geological investigations, historical research and comprehensive analysis. On the basis of its characteristics and activity, the fault can be divided into three sections, namely eastern, central and western. The eastern and western sections display normal slip. Intense deformation has occurred along the two sections during the Quaternary; however, no deformation has occurred during the Holocene. The central section has experienced significant high–angle normal fault activity during the Quaternary, including the Holocene. Holocene alluvial fans and loess cut by the fault have been identified at the mouths of many stream valleys of the Huashan Mountains along the central section of the Huashan piedmont fault zone. Of the three sections of the Huashan piedmont fault, the central section is the most active and was very active during the late Quaternary. The rate of normal dip–slip was 1.67–2.71±0.11 mm/a in the Holocene and 0.61±0.15 mm/a during the Mid–Late Pleistocene. As is typical of normal faults, the late Quaternary activity of the Huashan piedmont fault has produced a set of disasters, which include frequent earthquakes, collapses, landslides, mudslides and ground fissures. Ground fissures mainly occur on the hanging–wall of the Huashan piedmont fault, with landslides, collapses and mudslides occurring on the footwall.
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2015,89(3):715-725, DOI:
Abstract:
Re-equilibration of fluid inclusions in crystals takes place by loss or gain of solvents and solutes from fluid inclusions and by changes in their volumes. Volume change of fluid inclusions are primarily dictated by elastic properties and available slip planes of host crystals. In the present study, the phase-behavior of fluids entrapped in co-precipitated calcite and barite is studied. While calcite contains only biphase fluid inclusions, barite has predominantly monophase fluid inclusions. Fluid inclusion petrography, microthermometry and leachate analysis are used to establish the nature of entrapped fluids and entrapment temperature is substantiated through independent sulfur isotope geothermometry using coexisting barite and pyrite. Phase transitions in the monophase fluid inclusions in barite are explained in terms of over-pressuring of fluids in these fluid inclusions relative to fluids entrapped in calcite owing to the low bulk modulus of barite.
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2021,95(3):1056-1056, DOI: 10.1111/1755-6724.14310
Abstract:
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ZHANG Gang, WANG Xuben, FANG Hui, GUO Ziming, ZHANG Zhaobin, LUO Wei, CAI Xuelin, LI Jun, LI Zhong, WU Xing
2015,89(2):531-541, DOI:
Abstract:
The Panxi region is located in the frontal zone of positive squeezing subduction and side squeezing shearing between the Indian plate and the Eurasian plate. The long-period magnetotelluric (LMT) and broadband magnetotelluric (MT) techniques are both used to study the deep electrical conductivity structure in this region; magnetic and gravity surveys are also performed along the profile. According to the 2-D resistivity model along the Yanyuan-Yongshan profile, a high-conductivity layer (HCL) exists widely in the crust, and a high-resistivity block (HRB) exists widely in the upper mantle in general, as seen by the fact that a large HCL exists from the western Jinpingshan tectonic zone to the eastern Mabian tectonic zone in the crust, while the HRB found in the Panxi tectonic zone is of abnormally high resistivity in that background compared to both sides of Panxi tectonic zone. In addition, the gravity and magnetic field anomalies are of high value. Combined with geological data, the results indicate that there probably exists basic or ultrabasic rock with a large thickness in the lithosphere in the Panxi axial region, which indicates that fracture activity once occurred in the lithosphere. As a result, we can infer that the high-resistivity zone in the Panxi lithosphere is the eruption channel for Permian Emeishan basalt and the accumulation channel for basic and ultrabasic rock. The seismic sources along the profile are counted according to seismic record data. The results indicate that the most violent earthquake sources are located at the binding site of the HRB and the HCL, where the tectonic activity zone is generally acknowledged to be; however, the earthquakes occurring in the HCL are not so violent, which reflects the fact that the HCL is a plastic layer, and the fracture threshold of a plastic layer is low generally, making high stress difficult to accumulate but easy to release in the layer. As a result, a higher number of smaller earthquakes occurred in the HCL at Daliangshan tectonic zone, and violent earthquakes occurred at the binding site of high- and low-resistivity blocks at the Panxi tectonic zone.