松南十屋断陷深部地层层序的识别与划分  

Classification and Identification of Sequences in Deep Strata of Shiwu Fault Depression

作　　者：赵勇刚[1] 

机构地区：[1]中国地质大学,武汉430074

出　　处：《重庆科技学院学报（自然科学版）》2008年第2期10-12,共3页Journal of Chongqing University of Science and Technology：Natural Sciences Edition

摘　　要：根据层序地层学理论,综合应用测井、露头、岩芯及地震剖面等资料建立十屋断陷的层序地层格架。根据识别出的层序界面标志,十屋断陷深部断陷期可划出3个二级层序:初始裂陷期层序组、快速裂陷期层序组和裂陷萎缩期层序组。在裂陷期层序中可以划出5个三级层序,自下而上为:火石岭组层序、沙河子组层序、营一层序、营二层序和登楼库组层序。According to the theory of sequence stratigraphy, it establishes the sequence stratigraphic framework of Shiwu fault depression according to well Logging, out crop and core data. The deep strata of Shiwu fault depression can be divided into three second-order sequences of initial rifting period sequence, rapid rifting period sequence and atrophic rifting period sequence according to the sequence boundary marks that have been identified. In these rifting period sequences, the deep strata can be divided into five third-order sequences.It including Huoshiling formation sequence, Shahezi formation sequence, Ying＇yi sequence, Yinger sequence and Denglouku formation sequence from the lower layer to the upper layer.

关 键 词：十屋断陷 深部地层 层序识别 

分 类 号：TE121[石油与天然气工程—油气勘探]