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东天山红柳河地区蛇绿岩U-Pb同位素年龄
引用本文:于福生,李金宝,王涛.东天山红柳河地区蛇绿岩U-Pb同位素年龄[J].地球学报,2006,27(3):213-216.
作者姓名:于福生  李金宝  王涛
作者单位:中国石油大学,石油天然气成藏机理教育部重点实验室,北京,102249;长安大学资源学院,陕西西安,710054;中国地质科学院地质研究所,北京,100037
基金项目:国土资源部1∶5万《红柳河站幅》、《芦苇井幅》和区域地质调查项目[甘地勘地发(1996)17号]
摘    要:采用锆石U-Pb方法对东天山红柳河蛇绿岩中辉长岩进行了测试,得到206Pb/238U表面年龄加权平均值为425.5±2·3Ma,代表辉长岩的侵入年龄,说明红柳河蛇绿岩形成于早志留世,相当于文罗克世(Wenlock)哥利顿期(Gleedonian)。这一年龄结果表明早志留世中天山结晶基底已开始从塔里木板块北缘分离出去形成离散地体。

关 键 词:东天山  红柳河  蛇绿岩  U-Pb同位素年龄

The U-Pb Isotopic Age of Zircon from Hongliuhe Ophiolites in East Tianshan Mountains, Northwest China
YU Fu-sheng,LI Jin-bao and WANG Tao.The U-Pb Isotopic Age of Zircon from Hongliuhe Ophiolites in East Tianshan Mountains, Northwest China[J].Acta Geoscientia Sinica,2006,27(3):213-216.
Authors:YU Fu-sheng  LI Jin-bao and WANG Tao
Institution:Key Laboratory for Hydrocarbon Accumulation Mechanism, Ministry of Education, University of Petroleum, Beijing, 102249;Department of Resource, Chang an University, Xi'an, Shaanxi, 710054;Institute of Geology, GAGS, 100037
Abstract:The U-Pb isotopic age of zircon from gabbro in Hongliuhe ophiolites is about 425.5±2.3 Ma. This age that can be considered to be the formation time of the gabbro shows that the ophiolites were formed in Early Silurian, corresponding to Gleedonian period of Wenlock. The result indicates that the central Tianshan Mountains were separated from the Tarim plate and formed a discrete terrain in Early Silurian.
Keywords:East Tianshan Mountains  Hongliuhe area  ophiolites  U-Pb isotope age
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