新疆阿尔金地区长沙沟一带奥陶纪侵入岩及其演化特征

董洪凯, 郭金城, 陈海燕, 提振海, 刘广, 刘思林, 薛鹏远, 邢伟伟. 新疆阿尔金地区长沙沟一带奥陶纪侵入岩及其演化特征[J]. 西北地质, 2014, 47(4): 73-87.
引用本文: 董洪凯, 郭金城, 陈海燕, 提振海, 刘广, 刘思林, 薛鹏远, 邢伟伟. 新疆阿尔金地区长沙沟一带奥陶纪侵入岩及其演化特征[J]. 西北地质, 2014, 47(4): 73-87.
DONG Hong-kai, GUO Jin-cheng, CHEN Hai-yan, TI Zhen-hai, LIU Guang, LIU Si-lin, XUE Peng-yuan, XING Wei-wei. Evolution Characteristics of Ordovician Intrusive Rock in Changshagou of Altun Region[J]. Northwestern Geology, 2014, 47(4): 73-87.
Citation: DONG Hong-kai, GUO Jin-cheng, CHEN Hai-yan, TI Zhen-hai, LIU Guang, LIU Si-lin, XUE Peng-yuan, XING Wei-wei. Evolution Characteristics of Ordovician Intrusive Rock in Changshagou of Altun Region[J]. Northwestern Geology, 2014, 47(4): 73-87.

新疆阿尔金地区长沙沟一带奥陶纪侵入岩及其演化特征

  • 基金项目: 中国地质调查局基础调查项目"新疆阿尔金地区1:5万J45E012015等六幅区调"(1212011085033)

Evolution Characteristics of Ordovician Intrusive Rock in Changshagou of Altun Region

  • 新疆阿尔金地区长沙沟一带发育的侵入岩岩石类型包括辉石岩、辉长岩、辉绿辉长岩、石英闪长岩和石英二长闪长岩.野外地质特征和LA-ICP-MS锆石U-Pb测年结果显示就位时代均为奥陶纪.其中基性-超基性侵入岩具有幔源型特征;中-酸性侵入岩显示I型和地S型双重特征,其岩浆主要来源于上地幔,在岩浆上侵过程中同化混染了部分壳源物质,使其具有壳幔混合源的岩浆性质.基性-超基性侵入岩形成于超大陆裂解构造环境,系与大陆裂谷或深大断裂有关的深成岩浆作用的产物,中酸性侵入岩是汇聚阶段的产物.
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出版历程
收稿日期:  2014-06-17
修回日期:  2014-10-24
刊出日期:  2014-12-15

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