2024 06 v.54 961-974
鄂尔多斯盆地寒武纪沉积演化及天然气成藏条件分析
基金项目(Foundation):
陕西省自然科学基础研究计划项目(2021JM-158);
国家科技重大专项(2011ZX05005-004-07HZ);
中央高校基本科研业务费资助项目(0009-2014G1271062)
邮箱(Email):
DOI:
10.16152/j.cnki.xdxbzr.2024-06-003
中文作者单位:
长安大学地球科学与资源学院/土地工程学院;西北大学地质学系;
摘要(Abstract):
基于多年来对鄂尔多斯盆地寒武纪的研究成果，在大量野外剖面观察、钻井及岩心资料分析的基础上，对寒武纪地层划分、沉积体系类型、沉积演化特征及成藏条件进行研究。研究表明，研究区寒武系发育滨岸潮坪、碳酸盐台地、台地边缘3类沉积体系，鄂尔多斯盆地寒武纪为稳定大陆边缘陆表海沉积，由内向外表现为台内局限潮坪—台外开阔台地—台缘鲕粒滩—台前斜坡的构造古地理格局，沉积演化经历了早寒武世滨岸潮坪、中寒武世局限-开阔台地、晚寒武世局限-蒸发台地3个阶段，构成一个完整的演化旋回。研究认为，鄂尔多斯盆地寒武纪不发育深水沉积，烃源岩整体发育较差。晚寒武世—早奥陶世的怀远运动造成中央古隆起的形成，影响了晚寒武世的沉积格局，并且控制了中上寒武统的白云岩化作用及岩溶储层的发育。
关键词(KeyWords):
沉积体系;沉积演化;成藏条件;寒武纪;鄂尔多斯盆地
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基本信息:
DOI：10.16152/j.cnki.xdxbzr.2024-06-003
中图分类号:P618.13
引用信息:
[1]陈强,李文厚,李智超等.鄂尔多斯盆地寒武纪沉积演化及天然气成藏条件分析[J].西北大学学报(自然科学版),2024,54(06):961-974.DOI:10.16152/j.cnki.xdxbzr.2024-06-003.
基金信息:
陕西省自然科学基础研究计划项目(2021JM-158); 国家科技重大专项(2011ZX05005-004-07HZ); 中央高校基本科研业务费资助项目(0009-2014G1271062)