石油与天然气地质 ›› 2023, Vol. 44 ›› Issue (3): 764-777.doi: 10.11743/ogg20230318
吴冬1,2(), 邓虎成1,2(), 熊亮3, 曹凯旋2, 董晓霞3, 赵勇3, 魏力民3, 王同3, 马若龙1,2
收稿日期:
2022-12-31
修回日期:
2023-04-07
出版日期:
2023-06-01
发布日期:
2023-06-05
通讯作者:
邓虎成
E-mail:lisandpw@163.com;denghucheng@cdut.cn
第一作者简介:
吴冬(1987—),男,博士、副研究员,沉积学和储层地质学。E?mail: 基金项目:
Dong WU1,2(), Hucheng DENG1,2(), Liang XIONG3, Kaixuan CAO2, Xiaoxia DONG3, Yong ZHAO3, Limin WEI3, Tong WANG3, Ruolong MA1,2
Received:
2022-12-31
Revised:
2023-04-07
Online:
2023-06-01
Published:
2023-06-05
Contact:
Hucheng DENG
E-mail:lisandpw@163.com;denghucheng@cdut.cn
摘要:
四川盆地及其周缘下寒武统筇竹寺组页岩气资源丰富,是重要的页岩气产气层段之一。由于该套地层埋藏深、资料少且地质条件复杂,对其开展的层序地层研究较为薄弱,这严重制约了后续研究和生产。首先对四川盆地及其周缘早寒武世构造-沉积背景开展研究,在此基础上结合岩性、颜色、测井曲线、微量元素、古生物和地震反射同相轴等特征,对麦地坪组-筇竹寺组层序地层开展研究,提出层序划分思路,将麦地坪组-筇竹寺组从下往上依次划分为4个Ⅲ级层序。进而厘清层序地层空间分布规律,建立受全球板块张性活动控制的四川盆地及其周缘麦地坪组-筇竹寺组“早期窄盆差异沉积,后期广盆稳定分布”的层序演化模式。该演化模式对深化认识四川盆地寒武纪构造-沉积格局、推动沉积成藏等地质研究及促进深部页岩气勘探开发具有一定意义。
中图分类号:
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