准噶尔盆地南缘四棵树凹陷超深层构造演化与油气成藏过程
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本文为中国石油“十四五” 基础性与前瞻性项目(编号 2023ZZ0206,2021DJ0303,2021DJ0203)和国家科技重大专项(编号 2016ZX05003- 002)资助的成果


Ultra- deep tectonic evolution and hydrocarbon accumulation process in the lower play of Sikeshu sag, southern Junggar basin, western China
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    摘要:

    准噶尔盆地南缘下组合近年取得了重要勘探突破,随着勘探持续深化,在工业油气流圈闭附近的构造却钻探失利,下组合区域差异较大,成藏过程复杂。通过对高泉地区构造进行平衡地质剖面恢复,结合流体包裹体、埋藏史、热史和油气运聚数值模拟研究,揭示了高泉地区下组合的构造演化与成藏过程,并分析了部分井失利的原因。结果表明,高泉构造在前侏罗纪已经存在,为一宽缓古隆起,新生代早期受喜马拉雅造山运动影响,分割为若干断块构造,分割后的圈闭成藏过程具有差异性。高泉构造总体经历了3期油气充注和晚期的调整改造:第一期为中新统塔西河组沉积时期(约16 Ma)的低熟原油充注,对应包裹体荧光为黄色;第二期为独山子组沉积中期的成熟原油充注(约7 Ma),对应的是石英颗粒愈合缝内蓝色、蓝白色荧光油包裹体;第三期为上新世(约3 Ma)以来的天然气充注,天然气来源主要为四棵树凹陷,高泉地区本地烃源岩主体并未进入生气阶段。四棵树凹陷近端和远端圈闭成藏潜力和勘探远景具有较大差别,凹陷周边圈闭晚期多经历改造和调整,近端圈闭具有距离油源近、供烃充足等优势,应作为优先勘探目标,远端圈闭改造后油气源补充不足,具有较大勘探风险。

    Abstract:

    Recent years have witnessed significant advancements in the exploration of deep- seated reservoir plays within the southern margin of the Junggar basin. Despite these successes, drilling operations in structures adjacent to industrial petroleum traps have resulted in a number of unsuccessful ventures. This study investigates the tectonic evolution and hydrocarbon accumulation processes of the deep play in the Gaoquan area to understand the causes behind these drilling failures. A comprehensive approach, incorporating the restoration of the balanced geological profile, fluid inclusion analysis, burial and thermal history reconstructions, and numerical simulation techniques, provides a detailed understanding of the structural development and hydrocarbon migration in the Gaoquan area. The results show that the Gaoquan structure originated as a wide, gentle paleo- uplift during the pre- Jurassic era. The Himalayan orogeny in the early Cenozoic resulted in its division into several fault- block structures, leading to distinct trapping and accumulation processes. The Gaoquan structure underwent three distinct stages of hydrocarbon charging and subsequent modification. During the deposition of the Miocene Taxihe Formation (16 Ma), the initial stage involved the charging of low- maturity crude oil, as evidenced by yellow fluorescence in inclusions. The second stage, coinciding with the middle Dushanzi Formation (7 Ma), witnessed the charging of mature crude oil, characterized by blue and blue- white inclusions observed in quartz grain healing fractures. The final stage, commencing during the Pliocene (3 Ma), involved the charging of natural gas, primarily sourced from the Sikeshu sag, as the local source rock in the Gaoquan area has not yet reached the gas generation window. The proximity of the Gaoquan structure to the Sikeshu sag significantly influences its trappotential and overall exploration prospects. Traps surrounding the sag have undergone significant reformation and adjustment during later stages. Proximal traps, characterized by their proximity to oil sources and abundant hydrocarbon supply, present the most favorable exploration targets, highlighting their potential for successful hydrocarbon discoveries.

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吴海,卓勤功,柳少波,张亚丽,鲁雪松,张梓煜,刘慧.2024.准噶尔盆地南缘四棵树凹陷超深层构造演化与油气成藏过程[J].地质学报,98(7):2216-2232.
WU Hai, ZHUO Qingong, LIU Shaobo, ZHANG Yali, LU Xuesong, ZHANG Ziyu, LIU Hui.2024. Ultra- deep tectonic evolution and hydrocarbon accumulation process in the lower play of Sikeshu sag, southern Junggar basin, western China[J]. Acta Geologica Sinica,98(7):2216-2232.

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  • 收稿日期:2023-08-21
  • 最后修改日期:2023-10-14
  • 录用日期:2023-10-17
  • 在线发布日期: 2024-07-24