Origin of Overpressure and Its Influence on Hydrocarbon Leakage in Mosuowan Uplift of the Junggar Basin, NW China

IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2024-11-25 DOI:10.1002/gj.5097
Xiujian Ding, Guojian You, Ablimit Yiming, Hailei Liu, Wenlong Jiang, Zhe Cao, Ming Zha, Jiangxiu Qu
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Abstract

The Junggar Basin is one of the main petroliferous basins in Western China. The Mosuowan Uplift, located in the central part of the Junggar Basin, is a favourable hydrocarbon accumulation zone. The overpressure is widely developed in the strata below the Jurassic, and the pressure coefficient gradually increases with the buried depth, up to 2.15. Based on the multi-logging combination method, Bowers method, sonic velocity–density cross-plot method and combined with geological setting, using porosity data of sandstone, geochemical data of source rocks, acoustic transit time -resistivity cross plots and so on, the origins of overpressure in each stratum of the Mosuowan Uplift are analysed. The results show that disequilibrium compaction, pressure transfer and tectonic compression are the main reasons for the development of deep overpressure. Disequilibrium compaction is considered to be an important reason for overpressure in Jurassic, Triassic, Upper Permian Upper Wuerhe Formation and Middle Permian Lower Wuerhe Formation due to the development of multiple sets of mudstone in deep strata. The Jurassic is charged by deep overpressure fluid, and the pressure transfer also has a significant contribution to the overpressure of Jurassic. The tectonic inversion occurred in the central part of the basin at the end of the Early Permian, and the overpressure in the Middle Permian Xiazijie Formation was closely related to tectonic compression. The hydrocarbon generation of the Permian and Jurassic source rocks has little contribution to the overpressure of the Mosuowan Uplift due to the poor source rock. The Mosuowan Uplift is an inherited anticline, adjacent to hydrocarbon generation sag, which is the dominant direction of oil and gas migration, but drilling confirmed that the deep reservoir is water layer. Comprehensive analysis of maturity parameters, logging fluorescence show and quantitative fluorescence analysis indicates that overpressure caused oil and gas leakage and destroyed hydrocarbon reservoirs.

准噶尔盆地莫索湾隆起超压成因及其对油气泄漏的影响
准噶尔盆地是中国西部主要含油气盆地之一。摩梭湾隆起位于准噶尔盆地中部,是一个有利的油气成藏带。侏罗系以下地层普遍发育超压,压力系数随埋深逐渐增大,最高可达2.15。基于多次测井组合法、鲍尔斯法、声速密度交叉图法,结合地质背景,利用砂岩孔隙度资料、烃源岩地球化学资料、声透射时电阻率交叉图等资料,分析了莫索湾隆起各层超压成因。结果表明,不平衡压实作用、压力传递作用和构造挤压作用是深层超压形成的主要原因。侏罗系、三叠系、上二叠统上乌尔河组和中二叠统下乌尔河组深层发育多套泥岩,不平衡压实作用被认为是形成超压的重要原因。侏罗系受深部超压流体充注,压力传递对侏罗系超压也有重要贡献。早二叠世末盆地中部发生构造反转,中二叠世下子街组超压与构造挤压密切相关。二叠系和侏罗系烃源岩由于烃源岩质量差,对莫索湾隆起的超压贡献较小。摩梭湾隆起为继承背斜,毗邻生烃凹陷,是油气运移的主导方向,但钻探证实深层储层为水层。综合分析成熟度参数、测井荧光显示和定量荧光分析表明,超压导致油气泄漏,破坏油气藏。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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