石油与天然气地质 ›› 1991, Vol. 12 ›› Issue (1): 52-57.doi: 10.11743/ogg19910106

• 论文 • 上一篇    下一篇

层序地层学理论用于我国断陷盆地分析中的问题

徐怀大   

  1. 中国地质大学, 北京
  • 收稿日期:1989-06-26 出版日期:1991-03-25 发布日期:2012-01-16

PROBLEMS IN ANALYSIS OF FAULTED BASINS OF CHINA BASED ON SEQUENCE STRATIGRAPHIC THEORY

Xu Huaida   

  1. China University of Geosciences, Beijing
  • Received:1989-06-26 Online:1991-03-25 Published:2012-01-16

摘要:

层序地层学的理论基础是海平面周期性变化控制了旋回性沉积层序的产生。沉积层序内部具有一定规律分布的体系域,对油气勘探具有特别重要的意义。这一理论原则上适用于中国东部中新生代箕状凹陷的盆地分析,但应解决几个难题,以建立自己的层序模式。

关键词: 海面升降, 层序, 体系域

Abstract:

The basic principle of sequence stratigraphic theory is the eustatic sea level changes which control the occurrence of cyclic depositional successions within a basin. System tracts within any sequence have a specific stratul pattern and are significant for oil and gas exploration. Most of Mesozoic and Cenozoic depressions in the east part of China are faulted basins (half grabens) filled by more than one cyclic sequences and ought to be analyzed based on the theory of sequence stratigraphy regardless they are marine in originor not. However, some difficulties must be solved and some of their own specific patterns must be esteblished before this theory can be used because of many inland faulted basins in East China had been linked up with the open sea occasionally, and their stratal patterns are different from the Vail's one as the result of abundant sediments have been supplied from peripheral areas surrounding the basins.