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科学通报  2014 

孔兹岩系——贺兰山中段赵池沟岩组碎屑锆石LA-ICP-MS锆石U-Pb年代学、Hf同位素组成及其地质意义

DOI: 10.1360/csb2014-59-7-593, PP. 593-604

Keywords: 赵池沟岩组,孔兹岩系,贺兰山,华北克拉通,锆石Hf同位素

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Abstract:

对贺兰山中段古元古代赵池沟岩组剖2两块变质沉积岩样品中的碎屑锆石进行了U-Pb定年和Hf同位素研究.研究认为赵池沟岩组为华北克拉通孔兹岩系的一部分,其成岩时间为1.96Ga;碎屑锆石年龄谱显示赵池沟岩组具有和孔兹岩带东缘相同的物源属性,孔兹岩带内部古老岩浆活动是孔兹岩系沉积的主要物源基础;变质锆石数据支持华北克拉通孔兹岩带发生过两期变质作用,早期变质作用发生在约1.96~1.95Ga,晚期变质作用发生在约1.87Ga;Hf同位素数据表明西部陆块在2.5~2.3Ga有地壳增生.

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