Discovery of the Carboniferous in the Yanghe(Wushan)-Gucheng(Lixian)area and its geological significance

PEI Xianzhi 1,GUO Junfeng 1,LI Yong 1,DING Saping 2,SU Chunqian 1,HU Bo 1

2003 Vol. 22, No. 7

Article Contents

Article navigation > Geological Bulletin of China > 2003 > 22(7): 494-499

Next Article Previous Article

PEI Xianzhi 1,GUO Junfeng 1,LI Yong 1,DING Saping 2,SU Chunqian 1,HU Bo 1. Discovery of the Carboniferous in the Yanghe(Wushan)-Gucheng(Lixian)area and its geological significance[J]. Geological Bulletin of China, 2003, 22(7): 494-499.

Citation:

PEI Xianzhi 1,GUO Junfeng 1,LI Yong 1,DING Saping 2,SU Chunqian 1,HU Bo 1. Discovery of the Carboniferous in the Yanghe(Wushan)-Gucheng(Lixian)area and its geological significance[J]. Geological Bulletin of China, 2003, 22(7): 494-499.

Discovery of the Carboniferous in the Yanghe(Wushan)-Gucheng(Lixian)area and its geological significance

PEI Xianzhi 1,GUO Junfeng 1,LI Yong 1,DING Saping 2,SU Chunqian 1,HU Bo 1

Revised Date: 10 March 2003

Publish Date: 15 July 2003

Abstract

Abstract

Through regional geological survey,a sequence of Carboniferous sedimentary strata is divorced from the strata originally assigned to the Upper Devonian Dacaotan Group and Middle Devonian Shujiaba Group in the Yanghe(Wushan)-Gucheng(Lixian)area in the West Qinling.According to conodont ,coral and foraminifera fossils discovered,the geological age of this sequence of sedimentary strata is Early Carboniferous.
- Carboniferous,strata,fossil,Tianshui area,West Qinling orogenic belt,

FullText(HTML)