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新疆菁布拉克基性超基性岩带的Sm-Nd同位素年龄
引用本文:倪守斌,满发胜,陈江峰.新疆菁布拉克基性超基性岩带的Sm-Nd同位素年龄[J].岩石矿物学杂志,1994,13(3):227-231.
作者姓名:倪守斌  满发胜  陈江峰
作者单位:中国科学技术大学地球和空间科学系
基金项目:国家“七五”重点科技攻关项目
摘    要:Sm-Nd矿物等时线定年结果表明,菁布拉克岩带基性超基性岩形成于320Ma,其形成时代晚于早石炭世早期的火山活动,是塔里木板块与巩乃斯微板块碰撞晚期拉张构造环境的产物。

关 键 词:Sm-Nd年龄,基性超基性岩,新疆

Sm-Nd Isotope Ages of Basic and Ultrabasic Rocks from the Qingbulak Belt,Xinjiang
Ni Shoubin,Man Fasheng,Chen Jiangfeng.Sm-Nd Isotope Ages of Basic and Ultrabasic Rocks from the Qingbulak Belt,Xinjiang[J].Acta Petrologica Et Mineralogica,1994,13(3):227-231.
Authors:Ni Shoubin  Man Fasheng  Chen Jiangfeng
Abstract:Basic and ultrabasic rocks were dated by the Sm-Nd mineral isochron technique.The results show that these rocks were formed at 320 Ma B.P.after the Early Carboniferous volcanism,being products in an extonsion tec-tonic setting at the late stage of collision between the Tarim plate and the Gongnaisi microplate.
Keywords:Sm-Nd isotope ages  basic and ulatrabasic rocks  Xinjiang
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