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四川龙门山中段上三叠统须家河组特征

苟宗海

沉积与特提斯地质2001,Vol.21Issue(1):93-101,9.
沉积与特提斯地质2001,Vol.21Issue(1):93-101,9.

四川龙门山中段上三叠统须家河组特征

The Upper Triassic Xujiahe Formation in the Longmen Mountain area, Sichuan

苟宗海1

作者信息

  • 1. 成都理工学院,
  • 折叠

摘要

Abstract

The N-S-elongated Upper Triassic Xujiahe Formation strata cover an area of 150 km2 and a thickness of more than 2851 m in the Dayi-Chongzhou-Dujiangyan-Wenchuan zone, Sichuan. After the surveying of the 1∶50000 Sanjiang Sheet and Wanjiaping Sheet from 1997 to 1999, the author subdivided the Formation into three members, with particular emphasis on lithology, stratigraphic boundary and correlation, biostratigraphy and chronostratigraphy. Two types of sedimentary environmerts are also discriminated:delta facies and fluvial facies.

关键词

须家河组/岩石特征/地层对比/沉积环境

分类

天文与地球科学

引用本文复制引用

苟宗海..四川龙门山中段上三叠统须家河组特征[J].沉积与特提斯地质,2001,21(1):93-101,9.

沉积与特提斯地质

OACSCD

1009-3850

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