PROTEROZOIC INTRACONTINENTAL RIFTING OF THE QINLING OROGENIC BELT: EVIDENCE FROM THE GEOCHEMISTRY OF SEDIMENTARY ROCKS

被引：0

作者：

高山

张本仁

谢千里

郭孝明

机构：

[1] Department of Geochemistry

[2] China University of Geosciences

[3] PRC

[4] Wuhan 430074

来源：

Chinese Science Bulletin | 1991年 / 11期

关键词：

Qinling Orogenic Belt; Proterozoic intracontinental rifting; graywacke geochemistry;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

Ⅰ. INTRODUCTIONThe Proterozoic tectonic nature of the Qinling Orogenic Belt has fundamental importance in understanding the evolutionary history of the Qinling Belt and the North China and Yangtze (South China) cratons, where the Qinling Group plays a crucial role. Although there is a consensus that this group was mostly of the early Proterozoic age, much controversy still remains on its tectonic environment of formation.

引用

页码：920 / 923

页数：4

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