四川盆地开江—梁平海槽东南台缘带 走滑断裂特征及其控藏作用

作    者:吴永宏1,2,刘嘉伟1,冯亮2,庞艳超1,唐青松2,刘晓旭1,邬光辉1
单    位:1 西南石油大学地球科学与技术学院;2 中国石油西南油气田公司重庆气矿
基金项目:
摘    要:
开江—梁平海槽周缘二叠系—三叠系礁滩型气藏是四川盆地天然气勘探开发的重点领域,但深层(>4 500 m) 碳酸盐岩储层致密,制约了天然气藏的高效勘探与开发。基于重新处理的三维地震资料,开展走滑断裂的地震识别, 研究走滑断裂的构造特征,并结合钻井资料分析走滑断裂控藏作用与天然气富集规律。结果表明:开江—梁平海槽 地区发育一系列北西向的走滑断裂带,具有纵向分层、平面分段特征。剖面上走滑断裂多表现为直立型断裂与花状 断裂多层叠置,平面上断裂组合以斜列、侧列为主,形成线性构造、雁列构造、花状构造、马尾状构造等多种构造类型。 走滑断裂位移小、成熟度低,经历震旦纪末—早寒武世、前二叠纪、二叠纪—三叠纪等3期走滑断裂活动,具有连接生 长机制与继承性发育的特征。走滑断裂带裂缝发育,断裂及其相关溶蚀作用控制了优质储层的发育,可导致碳酸盐 岩渗透率增长超过1 个数量级、孔隙度增长超过1倍。走滑断裂不仅沟通海槽内的二叠系烃源岩,形成侧向运移优势 通道,而且可垂向连通深部烃源岩,形成断裂输导、复式成藏的多个含气层。开江—梁平海槽周缘台缘带及台内与走 滑断裂有关的深层碳酸盐岩气藏的勘探开发潜力巨大,是值得深入探索的有利新领域。
关键词:走滑断裂;成储;成藏;台缘带;开江—梁平海槽;四川盆地

Characteristics of the strike-slip faults and their effects on the gas accumulation in the southeastern Kaijiang-Liangping trough, Sichuan Basin

Author's Name: WU Yonghong, LIU Jiawei, FENG Liang, PANG Yanchao, TANG Qingsong, LIU Xiaoxu, WU Guanghui
Institution: 
Abstract:
Large quantity of the Permian-Triassic reef-shoal gas reservoirs have been discovered in Kaijiang-Liangping trough, which is an important area for increasing reserve and production in the Sichuan Basin. However, there are many dense reservoirs in deep strata more than 4 500 m in this area, so it is important to find fault-related "sweet spot" reservoirs for efficient gas reservoir exploration and development. Based on the 3D seismic reprocessing and interpretation of strike-slip faults, the structural characteristics of strike-slip faults are studied, and the reservoircontrolling factors and favorable exploitation directions related to the strike-slip faults are analyzed combining with drilling data. The results show that a series of NW-trending strike-slip faults are developed in Kaijiang-Liangping trough. The strike-slip faults are mainly of vertical and flower-like faults in the section, and oblique and lateral faults in the plane. There are multiple types of structures such as linear structure, en echelon structure, flower structure, horse-tail structure, which are characterized by vertical stratification and planar segmentation. The strike-slip fault has small displacement and low maturity, and has experienced the late Ediacaran-Early Cambrian, pre-Permian and Permian- Triassic activities, and has the characteristics of linkage growth mechanism and inherited evolution. It is shown that fractures are developed in strike-slip fault zone, and they subsequent increase carbonate rock’s permeability by more than one order of magnitude, and fracture-related dissolution porosity by more than one time, which play an important constructive role in carbonate reservoir. At the same time, the strike-slip faults not only form the dominant lateral migration channels connecting to the Permian source rocks in the trough, but also may vertically connect the deep Cambrian and Ordovician-Silurian source rocks to form multiple gas-bearing layers with the faults playing role of transportation and accumulation. The study suggests that there is great potential for natural gas exploration and development of the strike-slip fault-controlled gas reservoirs in the trough-platform margin and intra platform deep carbonate reservoirs in the Kaijiang-Liangping trough, which are favorable new domain that are worthy of further exploration and development in the Sichuan Basin.
Keywords: strike-slip fault; reservoir forming; hydrocarbon accumulation; platform margin; Kaijiang-Liangping trough; Sichuan Basin
投稿时间: 2023-10-08  
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