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东昆北成矿带冰沟南铜镍矿辉长岩地球化学特征
引用本文:闫佳铭,孙丰月,陈广俊,钱烨,李良,王超,何书跃.东昆北成矿带冰沟南铜镍矿辉长岩地球化学特征[J].世界地质,2016,35(3):729-737.
作者姓名:闫佳铭  孙丰月  陈广俊  钱烨  李良  王超  何书跃
作者单位:1. 吉林大学 地球科学学院,长春 130061; 2. 青海省第三地质矿产勘查院,西宁 810008
摘    要:通过对东昆北成矿带冰沟南铜镍矿辉长岩的全岩地球化学进行分析,以确定该岩体的岩石成因及其形成的构造环境。冰沟南辉长岩SiO_2的含量为49.72%~51.58%,岩石系列为钙碱性。稀土元素球粒陨石分配模式为轻稀土略富集型,δEu为1.26~1.54,轻微正Eu异常。岩石富集大离子亲石元素(LILE)Rb、Ba、K,相对亏损P。岩体中的La/Sm、Th/La和Nb/U比值显示在就位过程中经历了一定程度的地壳混染。研究认为,岩体的岩浆源区为亏损地幔。结合区域演化,认为岩体形成于碰撞后伸展的背景。

关 键 词:冰沟南铜镍矿  辉长岩  全岩地球化学  岩浆源区  构造环境  东昆北带

Geochemical characteristics of gabbro from Binggounan Cu- - Ni deposit in the north of eastern Kunlun metallogenic belt
YAN Jia-Ming,SUN Feng-Yue,CHEN Guang-Jun,JIAN Ye,LI Liang,WANG Chao,HE Shu-Yue.Geochemical characteristics of gabbro from Binggounan Cu- - Ni deposit in the north of eastern Kunlun metallogenic belt[J].World Geology,2016,35(3):729-737.
Authors:YAN Jia-Ming  SUN Feng-Yue  CHEN Guang-Jun  JIAN Ye  LI Liang  WANG Chao  HE Shu-Yue
Institution:1. College of Earth Sciences,Jilin University,Changchun 130061,China; 2. The Third Institution of Qinghai Geological Mineral Prospecting,Xining 810008,China
Abstract:In order to determine the petrogenesis and tectonic setting in the north of eastern Kunlun orogenic belt,the authors analyze the whole rock geochemical characteristics of gabbro in the Binggounan copper- nickel de- posit. The SiO 2 content of Binggounan gabbros is 49. 72% to 51. 58% and rock series are of calcium alkali. Chon- drte- normalized REE patterns are LREE- slight rich,δEu are 1. 26 ~ 1. 54 with slight Eu positive anomaly. The gabbros are enriched in large ion lithophile elements (LILE) Rb,Ba,K and relatively depleted in P. The La/ Sm,Th/La and Nb/U values suggest that rock masses have experienced some crustal contamination in the process of emplacement. Studies suggest that the primary magma deprived from a depleted mantle. Combining with regional tectonic evolution,the authors conclude that the gabbro formed in the post- collisional extension setting.
Keywords:Binggounan copper and nickel deposit  gabbro  whole rock geochemical characteristics  magma source  tectonic setting  north of eastern Kunlun orogenic belt
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