石油与天然气地质 ›› 1992, Vol. 13 ›› Issue (1): 37-46.doi: 10.11743/ogg19920104

• 论文 • 上一篇    下一篇

以构造地层学分析中国东部中、新生代构造-沉积特征

林宗满   

  1. 地质矿产部石油地质综合大队 湖北 江陵 434100
  • 收稿日期:1991-09-09 出版日期:1992-03-25 发布日期:2012-01-16

ANALYZING MESO-CENOZOIC TECTONIC-SEDIMENTARY CYCLES IN EAST CHINA ACCORDING TO TECTOSTRATIGRAPHY

Lin Zongman   

  1. Comprehensive Research Institute of Petroleum Geology, MGMR, Jiangling, Hubei
  • Received:1991-09-09 Online:1992-03-25 Published:2012-01-16

PDF (PC)

432

摘要：

根据构造地层学的原理和方法,将中国东部中、新生界划分为六个构造-沉积旋回,认为侏罗纪末幕运动是中、新生代最重要的、具有划分构造发展阶段意义的构造幕,从而把中、新生代构造演化史划分为三叠-侏罗纪、晚白垩世-第三纪两个阶段和早白垩世过渡阶段,并概述了每个阶段的基本构造特征。

关键词: 构造地层学, 中国东部, 中、新生代, 构造演化, 构造-沉积旋回, 白垩系, 第三系

Abstract:

According to the basic comception of tectostratigraphy,the author divided the Meso-Cenozoic Systems in East China into six tectonic-sedimentary cycles and proposed that the Lower Eogene should belong to Upper Cretaceous,Upper Triassic to Lower Jurassic in South China and the Nanyang Basin to Cretaceous.An important tectonic generation in the end of Jurassic is significant in dividing the tectonic evolution history into two stages,that is,Triassic-Jurassic stage and Late Cretaceous-Tertiary stage.Two huge tectonic sys-tems that developed in the stages derived from the same origin but different from each other.Extensive tectonic uncomformities could be found between the tectonic systems,thus resulting in two dimensional feature of Meso-Cenozoic Systems in East China.