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东秦岭松树沟蛇绿岩Sm-Nd同位素年龄的地质意义
引用本文:董云鹏, 周鼎武, 刘良, 张旗, 张宗清. 1997. 东秦岭松树沟蛇绿岩Sm-Nd同位素年龄的地质意义. 地质通报, 16(2).
作者姓名:董云鹏  周鼎武  刘良  张旗  张宗清
作者单位:1. 西北大学地质系;; 2. 中国科学院地质研究所;; 3. 中国地质科学院地质研究所
摘    要:东秦岭松树沟蛇绿岩主要由变质橄榄岩和变质玄武岩组成。变玄武岩全岩Sm Nd同位素等时年龄为(1030±46(2δ))Ma,INd=0.51161±5(2δ),εNd(t)=+5.7±0.2,代表蛇绿岩中玄武岩的形成年龄。这一年龄的确定,为探讨秦岭区中晚元古代的古构造格局提供了重要的证据

关 键 词:蛇绿岩   Sm-Nd等时线   松树沟   东秦岭

Sm Nd ISOTOPIC AGES OF THE SONGSHUGOU OPHIOLITE FROM THE EAST QINLING AND ITS GEOLOGICAL SIGNIFICANCE
1997. Sm Nd ISOTOPIC AGES OF THE SONGSHUGOU OPHIOLITE FROM THE EAST QINLING AND ITS GEOLOGICAL SIGNIFICANCE. Geological Bulletin of China, 16(2).
Authors:Dong Yunpeng  Zhou Dingwu  Liu Liang
Affiliation:1. Department of Geology, Northwest Univeristy, Xi’an, Shaanxi;; 2. Institute of Geology,Academia Sinica,Beijing;; 3. Institute of Geology,MGMR,Beijing
Abstract:The Songshugou ophiolite consists mainly of meta perdotite and meta basalt. Five whole rock samples of meta basalt give a Sm Nd isochron age of (1030±46 ) Ma with I Nd =0.51161±5 (2δ) and ε Nd (t) = +5.7±0.2, which may represent the formation age of the basalt. This age gives some important information about the Middle Late Proterozoic tectonic framework in the Qinling region.
Keywords:ophiolite   Sm Nd isochron   Songshugou   East Qinling
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