东昆仑埃坑德勒斯特二长花岗岩岩石地球化学特征及岩石成因

杨延乾, 李碧乐, 马延景, 谈艳, 保善斌, 李嘉泰, 于小亮, 王佳音. 东昆仑埃坑德勒斯特二长花岗岩岩石地球化学特征及岩石成因[J]. 西北地质, 2018, 51(1): 104-114.
引用本文: 杨延乾, 李碧乐, 马延景, 谈艳, 保善斌, 李嘉泰, 于小亮, 王佳音. 东昆仑埃坑德勒斯特二长花岗岩岩石地球化学特征及岩石成因[J]. 西北地质, 2018, 51(1): 104-114.
YANG Yanqian, LI Bile, MA Yanjing, TAN Yan, BAO Shanbin, LI Jiatai, YU Xiaoliang, WANG Jiayin. Geochemistry and Genesis of Monzonitic Granite from Aikengdelesite Area in East Kunlun, Qinghai[J]. Northwestern Geology, 2018, 51(1): 104-114.
Citation: YANG Yanqian, LI Bile, MA Yanjing, TAN Yan, BAO Shanbin, LI Jiatai, YU Xiaoliang, WANG Jiayin. Geochemistry and Genesis of Monzonitic Granite from Aikengdelesite Area in East Kunlun, Qinghai[J]. Northwestern Geology, 2018, 51(1): 104-114.

东昆仑埃坑德勒斯特二长花岗岩岩石地球化学特征及岩石成因

  • 基金项目: 青海省应用基础研究项目“东昆仑东段银多金属成矿规律研究与靶区优选”(2016-ZJ-719)

Geochemistry and Genesis of Monzonitic Granite from Aikengdelesite Area in East Kunlun, Qinghai

  • 埃坑德勒斯特铜(钼)矿是近年来在东昆仑地区发现的斑岩型铜(钼)矿,矿区位于东昆南复合拼贴带内,花岗斑岩及外围碎裂的二长花岗岩是主要的赋矿围岩。对二长花岗岩进行了岩石地球化学和Sr-Nd同位素研究,讨论了岩浆来源、岩石成因和构造背景。研究表明,岩石富硅,相对富钠贫钙和镁,属钙碱性过铝质系列岩石。岩石明显富集大离子亲石元素(K、Ba、Rb)和活泼的不相容元素(如Th、U),相对亏损高场强元素(Nb、Ta、P、Ti)。样品的ISr值为0.707 05~0.707 37,εNdt)为-2.2~-1.6,Rb/Sr为0.17~0.32,反映岩浆来源具壳幔混合特点。根据Y+Nb-Rb、La/Nb-Ba/Nb等判别图解及与俯冲有关的蛇绿岩带发育特征,表明该岩体形成于安第斯型活动大陆边缘环境。俯冲作用导致俯冲板片的流体降低熔点和直接交代地幔,使地幔部分熔融形成基性岩浆。幔源岩浆底侵作用提供热能,使基性下地壳物质部分熔融形成花岗质岩浆,其中混入了少量幔源岩浆。
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出版历程
收稿日期:  2017-01-20
修回日期:  2017-10-12
刊出日期:  2018-03-15

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