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鄂尔多斯盆地奥陶系盐下层系构造-沉积分异与烃源岩-储层分布规律

苏中堂 徐哲博 魏柳斌 师平平 张雷 任军峰 任静 吴浩文 朱梦涵

石油与天然气地质2026,Vol.47Issue(1):64-80,17.
石油与天然气地质2026,Vol.47Issue(1):64-80,17.DOI:10.11743/ogg20260105

鄂尔多斯盆地奥陶系盐下层系构造-沉积分异与烃源岩-储层分布规律

Tectonic-sedimentary differentiation and hydrocarbon source rock-reservoir distribution pattern of the Ordovician sub-salt sequence in the Ordos Basin

苏中堂 1徐哲博 2魏柳斌 2师平平 3张雷 4任军峰 3任静 4吴浩文 3朱梦涵4

作者信息

  • 1. 油气藏地质及开发工程国家重点实验室(成都理工大学),四川 成都 610059
  • 2. 成都理工大学沉积地质研究院,四川 成都 610059
  • 3. 低渗透油气田勘探开发国家工程实验室,陕西 西安 710018
  • 4. 中国石油长庆油田公司勘探开发研究院,陕西 西安 710018
  • 折叠

摘要

Abstract

The carbonate-evaporite system in the sub-salt sequence has been a key area for increasing oil and gas reserves and production.Its source rock-reservoir combination styles and distribution have become the key constraints on oil and gas exploration.Analyzing the development and distribution pattern of hydrocarbon source rock-reservoir in the sub-salt carbonate-evaporite system in the Ordos Basin,we explore the controlling factors.The results show that:the hierarchical"uplift-depression"structural pattern determines the sedimentary substrate variability,and the dry and wet paleoclimate changes alter the oceanic conditions,leading to sedimentary differentiation,which results in the formation of different carbonate-evaporite depositional sequences,and the development of various hydrocarbon source rocks and reservoirs.Paleo-uplifts and subordinate uplifts control the distribution of hydrocarbon source rocks for arid-climate argillaceous dolomites,and the paleo-depressions are favorable for the growth of hydrocarbon source rocks for wet-climate micrites;grainstone deposits are prone to developing in paleo-uplift and subordinate uplift zones,which are also a favourable habitat for benthic organisms.These zones are the dominant zones for the reflux of high-salinity brine in the process of the climate shifting from wet to arid,where the occurrence of dolomitization is widely seen,controlling the distribution of crystalline dolostone,grain dolostone,microbial dolostones and porphyritic dolostone reservoirs.Tectonic-sedimentary differentiation governs the distribution pattern of hydrocarbon source rocks and reservoirs in the carbonate-evaporite system.The slope zone around the Central paleo-uplift and the Wushenqi uplift and Shenmu-Mizhi low uplift zone adjacent to the paleo-depression have effective hydrocarbon source rock-reservoir combinations developed,favourable zones for oil and gas exploration in the sub-salt sequence.

关键词

古气候/构造-沉积分异/碳酸盐岩-蒸发岩体系/白云岩/深层-超深层/马家沟组/奥陶系/鄂尔多斯盆地

Key words

paleoclimate/tectonic-sedimentary differentiation/carbonate-evaporite system/dolostone/deep to ultra-deep reservoirs/Majiagou Formation/Ordovician/Ordos Basin

分类

能源科技

引用本文复制引用

苏中堂,徐哲博,魏柳斌,师平平,张雷,任军峰,任静,吴浩文,朱梦涵..鄂尔多斯盆地奥陶系盐下层系构造-沉积分异与烃源岩-储层分布规律[J].石油与天然气地质,2026,47(1):64-80,17.

基金项目

中国石油长庆油田创新联合体项目(2024D1JC06) (2024D1JC06)

中国石油攻关性应用性科技专项(2023ZZ16YJ01). (2023ZZ16YJ01)

石油与天然气地质

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