Sm-Nd ISOTOPIC SYSTEMATICS OF THE NE JIANGXI OPHIOLITE(NEJXO), SE MARGIN OF THE YANGTZE CRATON, SOUTH CHINA

被引：7

作者：

周国庆

赵建新

机构：

[1] PRC

[2] Canberra

[3] G. P. O. Box 4

[4] Nanjing University

[5] Department of Earth Sciences

[6] Research School of Earth Sciences

[7] Nanjing 210008

[8] A. C. T. 2601

[9] Australian National University

来源：

ChineseScienceBulletin | 1991年 / 16期

关键词：

Proterozoic ophilolite; Sm-Nd isotopes;

D O I：

暂无

中图分类号：

学科分类号：

摘要：

The ophiolite belt along the S.E. margin of the Yangtze craton(or platform), South China is commonly considered to be formed during the Sibao-Xuefeng orogenic cycle and interpreted to represent a Proterozoic suture or subduction zone. In contrast, Hsu et al. recently argued that this ophiolite belt represented a melange which was overthrust onto a foreland thrust belt during Mesozoic. To resolve this conflict and obtain better under-

引用

页码：1374 / 1379

页数：6