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西准噶尔色尔登花岗岩地球化学特征及其构造意义
引用本文:姚 超,第鹏飞,王金荣,何彦斌,张 伟,刘昆鑫,魏东伟.西准噶尔色尔登花岗岩地球化学特征及其构造意义[J].甘肃地质学报,2012(2):14-20.
作者姓名:姚 超  第鹏飞  王金荣  何彦斌  张 伟  刘昆鑫  魏东伟
作者单位:[1]兰州大学地质科学与矿产资源学院,甘肃兰州730000 [2]甘肃省国土资源厅,甘肃兰州730000
基金项目:本文为新疆维吾尔自治区国土资源厅国土大调查项目资助([2008]增01-01-01)
摘    要:本文在野外实地调查的基础上,分析研究了新疆西准噶尔色尔登花岗岩岩体的岩石组合类型和岩石地球化学特征。研究结果表明,色尔登岩体为晚石炭世后I型花岗岩,形成于后碰撞伸展背景下,物源为下地壳中基性物质的部分熔融,但形成时的地壳厚度较薄,部分熔融的热力来源为软流圈玄武质岩浆底侵作用。本文通过探讨西准噶尔晚石炭世花岗岩类形成时的构造环境、成因机制及构造意义,为西准噶尔地区晚石炭世地壳内部物质重新分配的过程研究提供了新的依据。

关 键 词:后碰撞  花岗岩  地球化学  构造意义  晚古生代  西准噶尔

Geochemical Characteristics and Tectonic Significance of Seerdeng granite in West Junggar
YAO Chao,DI Peng-fei,WANG Jin-rong,HE Yan-bin,ZHANG Wei,LIU Kun-xin and WEI Dong-wei.Geochemical Characteristics and Tectonic Significance of Seerdeng granite in West Junggar[J].Acta Geologica Gansu,2012(2):14-20.
Authors:YAO Chao  DI Peng-fei  WANG Jin-rong  HE Yan-bin  ZHANG Wei  LIU Kun-xin and WEI Dong-wei
Institution:1. School of Earth Sciences, Lanzhou University, Lanzhou 730000, China) 2. The Department of Land and Resources of Gansu Province, Lanzhou 730000, China)
Abstract:Based on the field study, this paper has carried out petrology and petro-geochemistry of Seerdeng granites in West Junggar, formed during the Late Paleozoic, formation mechanism and tectonic significance. The study results show that Seerdeng granite was I-type granites, which formed in a post-collisional extension setting, and resulted from the partial melting of basical substance of lower crust, with a circumstance of relativelt thin continental crust, and the the heat energy for partial melting was provided by the underplating of asthenosphere basaltic magmas. The study provides new evidence for Late Carboniferous crustal material and re-allocation process (crustal evolution) in the West Junggar.
Keywords:Post-collisional Granite  geochemistry  Tectonic Significance  Late Paleozoic  West Junggar
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