延安地区奥陶系马家沟组上组合膏盐岩成盐沉积演化模式研究
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本文为中国地质调查局项目(编号DD20190379、DD20160346)资助成果。


Study of the salt- formation and sedimentary evolution model of the Upper Ordovician Majiagou Formation in the Yan’an area
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    摘要:

    延安地区经过十余年油气勘探,在奥陶系马家沟组获得了一系列的突破,其中马家沟组上组合是天然气勘探的重要层位,该区是奥陶系碳酸盐岩- 膏盐岩共生体系的主要沉积区,其中马家沟组上组合马五43- 马五32膏盐沉积是海退蒸发环境的典型代表。本文基于延安气田奥陶系天然气勘探的最新进展,利用现场岩心观察、实验分析、钻井及测井资料,根据沉积构造、膏盐岩发育规模、岩性组合方式等,对研究区奥陶系马家沟组上组合膏盐岩的地质特征进行了详细的阐述,系统地总结了研究区马家沟组上组合膏盐岩的沉积背景及沉积相、建立了沉积演化模式,为延安气田膏盐岩研究提供基础资料。研究表明,在西高东低的沉积格局背景下,地层充填呈西薄东厚,南薄北厚的特点;自西南向东北依次为膏质白云岩- 膏岩- 盐岩沉积区;垂向发育三种岩石类型组合:Ⅰ型膏质白云岩- 硬石膏结核白云岩- 膏质白云岩- 泥云岩组合,Ⅱ型膏岩- 硬石膏结核白云岩- 膏质白云岩- 泥云岩组合,Ⅲ型盐岩- 膏岩- 硬石膏结核白云岩- 膏质白云岩组合;沉积环境为相对安静且低能的潟湖沉积模式。沉积环境演化为极强蒸发盐化→蒸发膏化→相对开放。研究成果为鄂尔多斯盆地其他地区奥陶系膏盐岩地质研究提供借鉴,对延安气田油气勘探具有重要指导意义。

    Abstract:

    Over a decade of oil and gas explorations in the Yan’an area have yielded a series of breakthroughs in documenting theupper Ordovician Majiagou Formation, an important layer for natural gas exploration.This is the main sedimentary area of the Ordovician carbonate- gypsum rock symbiotic system, in which the M543- M532 gypsum deposit of the upper Majiagou Formation is a typical representative of the regressive evaporative environment. Based on the latest results from the development of Ordovician gas exploration in the Yan’an gas field, utilizing datafromcore observations, experimental analysis, drilling and logging, and on the basis of sedimentary structure, the scale of gypsum- salt rock development, lithologic assemblage and the geological characteristics of gypsum- salt rock assemblage in the Majiagou Formation in the study area are elaborated. Finally, the sedimentary background, sedimentary facies and sedimentary evolution model of the assemblage gypsum- salt rocks in the Majiagou Formation in the study area are systematically summarized. The results indicate thatagainst the background of sedimentary pattern of high west and low east, stratum filling is characterized by thin west and thick east, thin south and thick north.The gypsum dolomite- gypsum- salt deposit area extends from southwest to northeast. Three types of rock assemblages were vertically developed: type I gypsum dolomite- anhydrite nodule dolomite- gypsum dolomite- mudstone assemblage; type II gypsum- anhydrite nodule dolomite- gypsum dolomite- mudstone assemblage; and type III salt- gypsum- anhydrite nodule dolomite- gypsum dolomite assemblage. It is a relatively quiet and low- energy lagoon sedimentary model. There is evolution of sedimentary environment into extreme evaporative salinization- evaporative gypsum- relative openness. The research results can be used as reference for geological research into the Ordovician gypsum salt rock in other areas of Ordos Basin and also provide important guidance for oil and gas exploration in the Yan’an gas field.

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吴海燕,梁婷,曹红霞,乔向阳,王凯,李克永,于珺,郭艳琴.2020.延安地区奥陶系马家沟组上组合膏盐岩成盐沉积演化模式研究[J].地质学报,94(12):3819-3829.
WU Haiyan, LIANG Ting, CAO Hongxia, QIAO Xiangyang, WANG Kai, LI Keyong, YU Jun, GUO Yanqin.2020. Study of the salt- formation and sedimentary evolution model of the Upper Ordovician Majiagou Formation in the Yan’an area[J]. Acta Geologica Sinica,94(12):3819-3829.

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  • 收稿日期:2019-10-30
  • 最后修改日期:2019-12-03
  • 录用日期:2020-01-03
  • 在线发布日期: 2020-01-03