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克孜勒塔格地区古元古代黑山梁片麻状辉长岩—二长花岗岩序列的特征分析
引用本文:谢渝,舒林,李新安. 克孜勒塔格地区古元古代黑山梁片麻状辉长岩—二长花岗岩序列的特征分析[J]. 资源环境与工程, 2012, 26(4): 331-338
作者姓名:谢渝  舒林  李新安
作者单位:1. 新疆地矿局 物化探大队,新疆昌吉,831100
2. 河南省地矿局 第二地质勘察院,河南许昌,461000
摘    要:在克孜勒塔格地区开展的1∶5万区域地质矿产调查工作,初步查明了此区古元古代变质花岗岩的岩石学、岩石化学等特征,对该期侵入岩的岩体成因及就位机制进行了探讨,并对其形成时代进行了推断。岩体侵位明显受线状构造("X"型剪裂隙)控制,说明该区域在地壳演化早期存在,岩体就位以构造扩展机制为主。其侵位时间为古元古代晚期。

关 键 词:克孜勒塔格  岩石学  岩石化学  岩体成因  就位机制

Characteristic of Palaeoproterozoic Heishanliang Gnessic Gabbro-Monzogranite Sequence in the Area of Keziletage
XIE Yu , SHU Lin , LI Xinan. Characteristic of Palaeoproterozoic Heishanliang Gnessic Gabbro-Monzogranite Sequence in the Area of Keziletage[J]. Resources Environment & Engineering, 2012, 26(4): 331-338
Authors:XIE Yu    SHU Lin    LI Xinan
Affiliation:1.Geophysical and Geochemical Party,Xinjiang Bureau of Geology and Mineral Resources Exploration and Development,Changji,Xinjiang,831100,China; 2.Second Institute of Geological and Mineral Exploration,Henan Bureau of Geology and Mineral Resource,Xuchang,Henan 461000)
Abstract:Based on the work of 1∶50 000 regional geological-mineral survey in Keziletage,it preliminarily finds out the petrology and petrochemistry of palaeoproterozoic meta-granitoid.This paper discusses the rock genetic and emplacement mechanism of the palaeoproterozoic intrusive rock,and deduces the formation age.Emplacement is significantly controlled by linear structure,indicating that the region exists in early stage of the crustal evolution.Emplacement time is Late paleoproterozoic.
Keywords:Keziletage  petrology  petrochemistry  genesis  emplacement mechanism
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