江汉盆地江陵凹陷盐构造类型及成因机制探讨
详细信息 本馆镜像全文    |  推荐本文 | | 获取馆网全文
摘要
根据钻井资料和地震剖面,分析了江陵凹陷盐构造特征和盐构造形成的动力条件,探讨了江陵凹陷盐构造类型、成因机制及演化。分析表明,江陵凹陷发育盐枕、盐背斜、盐脊三种盐构造类型;将盐构造活动划分为沙市组晚期-新沟嘴组沉积期为盐构造孕育阶段、荆沙期-荆河镇早期为盐构造生长阶段、古近纪末期-新近纪早期盐构造盐构造定型三个阶段;同时总结盐构造的活动对油气聚集成藏的影响。
According to drilling data and seismic profile, salt structure features, dynamic conditions of salt structure formation, its genetic mechanism and evolution have been discussed and analyzed in this paper. The analysis indicates three structural types, salt pillow, salt anticline and salt-apex, have been developed in Jiangling depression, which divides the salt tectonic activities into three stages. The sedimentary period of late Shashi formation-Xingouzui formation is the structural generation stage, the Jinsha period-Jinhezhen early period is he structral growth stage and the late Paleogene-early Neogene period is the structral formation stage. At the same time, the effect of salt structure activities on hydrocarbon accumulation has been summarized.
引文
[1]陈金荣.重新认识江陵凹陷荆沙组油气勘探前景[J].江汉石油职工大学学报,2012,(4):4-5.
    [2]王跃飞,王兰生.江陵凹陷底辟构造形成机制研究[J].地质灾害与环境保护,2002,11(3):51-54.
    [3]杨长清.江陵凹陷盐构造及与油气聚集关系[J].断块油气田,2004,11(3):4-6.
    [4]汤良杰,余一欣,陈书平,等.含油气盆地盐构造研究进展[J].地学前缘,2005,12(4):375-383.
    [5]高霞,谢庆宾.浅析膏盐岩发育与油气成藏的关系[J].石油地质与工程,2007,21(1):9-11.

版权所有:© 2023 中国地质图书馆 中国地质调查局地学文献中心