三叠纪嘉陵江期华蓥山同沉积断层的沉积、储层响应SYNDEPOSITIONAL TECTONIC ACTIVITIES IN THE HUAYINGSHAN FRACTURE BELT DURING THE TRIASSIC JIALING RIVER PHASE AND ITS IMPACT ON SEDIMENTATION AND RESERVOIR DEVELOPMENT
刘宏,孙振,李卓沛,李凌,聂勇,吴家杰,周小刚,谭秀成
摘要(Abstract)：
对于断裂带在地质历史时期活动特点的认识,因多期次、不同活动性质的叠加改造而难以确定。以四川盆地南部嘉陵江组为例,通过三叠纪嘉陵江期华蓥山断裂带两侧的沉积、储层的研究发现沉积、储层响应与断面倾向南东、东侧下降的观点矛盾。主要表现为:在非浅滩化的嘉三期,紧邻断裂带西北侧的下降盘地层异常增厚;浅滩化的嘉一晚期—嘉二1期,东南侧的泸州古隆起地区颗粒岩累计厚度较西北侧增厚;另外,断层东南侧的颗粒岩发育早期岩溶型储层,而在西北侧这类储层欠发育。结果表明在三叠纪嘉陵江期华蓥山断裂带的断面倾向北西,为西侧下降的同沉积正断层。
关键词(KeyWords)： 同沉积断层;沉积响应;储层响应;嘉陵江期;三叠纪;华蓥山断裂带;四川
基金项目(Foundation): 四川省重点学科建设项目(SZD0414)资助
作者(Author): 刘宏,孙振,李卓沛,李凌,聂勇,吴家杰,周小刚,谭秀成
DOI: 10.19839/j.cnki.dcxzz.2010.03.012
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