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Carbon Isotopic Evolution Characteristics and the Geological Significance of the Permian Carbonate Stratotype Section in the Northern Upper-Yangtze Region, Southern China

QU Hongjun LI Peng LUO Tengwen GUAN Liqun FAN Yuhai WANG Li

地质学报(英文版)2018,Vol.92Issue(6):2367-2381,15.
地质学报(英文版)2018,Vol.92Issue(6):2367-2381,15.

Carbon Isotopic Evolution Characteristics and the Geological Significance of the Permian Carbonate Stratotype Section in the Northern Upper-Yangtze Region, Southern China

Carbon Isotopic Evolution Characteristics and the Geological Significance of the Permian Carbonate Stratotype Section in the Northern Upper-Yangtze Region, Southern China

QU Hongjun 1LI Peng 1LUO Tengwen 1GUAN Liqun 1FAN Yuhai 2WANG Li1

作者信息

  • 1. State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China
  • 2. Remote Sensing Application Institute of ARSC, Xi'an 710069, China
  • 折叠

摘要

关键词

carbon isotope/mass extinction/eruption of Emeishan Flood Basalts/Permian/the Upper Yangtze region

Key words

carbon isotope/mass extinction/eruption of Emeishan Flood Basalts/Permian/the Upper Yangtze region

引用本文复制引用

QU Hongjun,LI Peng,LUO Tengwen,GUAN Liqun,FAN Yuhai,WANG Li..Carbon Isotopic Evolution Characteristics and the Geological Significance of the Permian Carbonate Stratotype Section in the Northern Upper-Yangtze Region, Southern China[J].地质学报(英文版),2018,92(6):2367-2381,15.

基金项目

This research was financially supported by The National Key Research Project of China (No.2016YFC0601003),Northwest University Graduate Innovation and Creativity Funds (YZZ17198) and the National Natural Science Foundation of China (Grants No.41390451 and No.41172101).We thank the anonymous reviewer and the Editor for their comments and suggestions,which significantly improved the quality of the manuscript,and we would also thank Prof.Yunpeng Dong and Prof.Jian Xu from Northwest University,China for their insightful discussions and suggestions. (No.2016YFC0601003)

地质学报(英文版)

OACSCDCSTPCD

1000-9515

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