四川盆地震旦系构造-沉积格局和天然气差异聚集OA
Tectonic-sedimentary framework and natural gas differential entrapment of the Sinian System in the Sichuan Basin,China
本文基于四川盆地最新的地质学-地球物理-地球化学的综合研究资料,针对灯影组油气勘探"一老一新"的 2个关键地质问题开展深入研究,即(1)震旦系灯影组沉积时的构造-沉积格局;(2)灯影组古气藏向现今气藏转换过程及现今气藏分布规律.结果表明:(1)四川盆地内受控于前震旦系北东走向岛弧基底古构造影响,在陡山沱组沉积期形成北东走向的宣汉—遂宁—峨眉古隆起;灯影组沉积时继承了陡山沱组沉积时的古隆起构造特征,但隆起面积缩小,形成北东走向的宣汉—开江古隆起.四川盆地在震旦纪主体处于弱挤压或构造中性状态,主要为古隆起形成演化阶段.前震旦系和震旦系陡山沱组在现今四川盆地范围内发育优质烃源岩和储集岩的可能性较小,四川盆地前震旦系的油气勘探前景应不大.(2)四川盆地晚白垩世构造隆升时灯影组古构造演化控制了灯影组古气藏内天然气沿其顶部不整合面发生盆地尺度的长距离大范围立体运移和差异聚集分布,而盆地周缘和盆地内保存条件被破坏的区域(气烟囱)则是启动天然气立体运移和差异聚集分布的主要动力.盆地内构造的低部位形成分气谷,分气谷两侧的天然气向盆地内构造高部位(即汇气岭或气烟囱)和盆地周缘造山带(气烟囱)运移,在其运移途中相关联的梯级圈闭聚集天然气形成局部构造-岩性气藏.构造作用形成的气烟囱、汇气岭和分气谷决定了灯影组现今天然气的区域分布.灯影组的天然气勘探应以构造(背景)圈闭气藏为主并以华蓥山以西地区为重点.
Based on comprehensive geological,geophysical,and geochemical data of Sichuan Basin,we conducted an in-depth investigation on two critical geological issues related to Sinian petroleum exploration:(1)the Sinian tectonic-sedimentary framework,and(2)the transformation from Sinian paleo-gas reservoirs to current reservoirs,based on their distribution patterns.Our results are summarized as follows:(1)The NE-trending Xuanhan-Suining-Emei paleo-uplift formed during Doushantuo Formation sedimentation in Sichuan Basin,influenced by pre-Sinian NE-trending arc basement structures.Dengying Formation inherited this tectonic framework but with reduced uplift dimensions,resulting in the NE-trending Xuanhan-Kaijiang paleo-uplift.During the depositional period of Doushantuo Formation and Dengying Formation in the Sinian System,Sichuan Basin was predominantly in a weakly compressional or tectonically neutral setting,representing a stage of paleo-uplift formation and evolution.Consequently,the likelihood that high-quality source rocks or reservoir rocks within the pre-Sinian and Sinian Doushantuo Formation are present in the present-day Sichuan Basin is minimal.Therefore,the petroleum exploration potential of the Pre-Sinian System in this region is limited.(2)The rapid tectonic uplift of Sichuan Basin during the Late Cretaceous governed basin-scale differential gas entrapment along the top unconformity of Dengying Formation,while the preservation-compromised zones(e.g.,gas chimneys)at the basin's periphery and interior acted as a critical switch for dynamic basin-wide readjustment of the natural gas.Structural lows within the basin developed gas-divergent valleys,and natural gas from both sides of these valleys migrated toward structural highs(gas-convergent ridges or gas chimneys)and orogenic belts at the basin's periphery(also gas chimneys).Associated contiguous traps along migration pathways accumulated gas,forming structural-lithological reservoirs.Tectonically induced gas chimneys,gas-convergent ridges,and gas-divergent valleys collectively govern the present-day gas distribution in Dengying Formation.Consequently,Sinian gas exploration should prioritize structural traps,focusing on the western areas of Huaying Mountains.
刘树根;赵晓丽;孙玮;郭冉;李泽奇;宋金民;邓宾;李智武;吴娟;叶玥豪
油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059||西华大学,成都 610039油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059中国石油川庆钻探工程有限公司地球物理勘探公司,成都 610213油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059油气藏地质及开发工程全国重点实验室(成都理工大学),成都 610059
天文与地球科学
四川盆地陡山沱组灯影组古隆起差异聚集深层油气
Sichuan BasinDoushantuo FormationDengying Formationpaleo-upliftdifferential entrapmentdeep-seated oil and gas
《成都理工大学学报(自然科学版)》 2026 (2)
203-224,22
国家科技重大专项(2025ZD1402500).
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