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现代地质 ›› 2019, Vol. 33 ›› Issue (04): 703-714.DOI: 10.19657/j.geoscience.1000-8527.2019.04.02

• 岩石学、矿物学、矿床学 • 上一篇    下一篇

西藏切穷地区早白垩世花岗岩年代学和地球化学特征及其构造环境

黄泽森1,2(), 江巴多吉3, 达瓦次仁3, 塔尔杰3   

  1. 1.成都理工大学 地球科学学院,四川 成都 610059
    2.四川省地质矿产勘查开发局二零七地质队,四川 乐山 614200
    3.西藏工程勘察施工集团有限责任公司,西藏 拉萨 850000
  • 收稿日期:2018-01-21 修回日期:2018-11-26 出版日期:2019-08-20 发布日期:2019-09-05
  • 作者简介:黄泽森,男,工程师,硕士研究生,1988年出生,矿物学、岩石学、矿床学专业,从事区域地质矿产调查工作。Email: 289700742@qq.com
  • 基金资助:
    中国地质调查局项目“冈底斯-喜马拉雅铜矿资源基地项目”(121201010000150014-10)

Geochemistry and Geochronology of Early Cretaceous Granitic Intrusions and Tectonic Setting of Qieqiong Area in Tibet,China

HUANG Zesen1,2(), JIANGBA Duoji3, DAWA Ciren3, TAER Jie3   

  1. 1. College of Earth Sciences, Chengdu University of Technology, Chengdu,Sichuan 610059, China
    2. No.207 Geological Team of Sichuan Geology and Mineral Resources Exploration Development Bureau, Leshan,Sichuan 614200, China
    3. Tibet Engineering Survey Construction Group Co. Ltd., Lhasa,Tibet 850000,China
  • Received:2018-01-21 Revised:2018-11-26 Online:2019-08-20 Published:2019-09-05

摘要:

西藏谢通门县切穷地区发育面积较广的早白垩世花岗岩岩体。为了进一步查明花岗岩的特征、侵入时代及其形成环境,对其进行了地质学、岩石地球化学及年代学研究。岩体LA-ICP-MS锆石U-Pb定年结果表明,研究区花岗岩岩体侵位年龄主要集中于(129.3±0.8)~(130.5±0.9) Ma,属早白垩世。从岩石地球化学特征来看,研究区花岗岩岩体具有高SiO2(73.19%~76.7%)、富碱(K2O+Na2O=7.81%~8.41%)特征,铝饱和指数(A/CNK)介于0.93~1.12之间,为强过铝质花岗岩;贫CaO(0.32%~7.31%)、MgO(0.01%~1.76%),显示明显的负铕(δEu=0.11~1.25)异常,富集Rb、Th、Nd元素,亏损Nb、Sr、P、Ti、K元素。从形成环境来看,研究区花岗岩具有明显的大陆碰撞环境的特征。研究认为,西藏切穷地区早白垩世花岗岩形成于同碰撞环境,但在后碰撞过程中地壳缩短增厚发生拆沉作用,玄武质岩浆岩底侵,经过中下地壳发生改造重熔形成的。

关键词: 锆石U-Pb定年, 岩石地球化学, 花岗岩, 冈底斯, 构造环境

Abstract:

A wide range of Early Cretaceous granitic intrusions were formed in the Qieqiong area in Tibet.To better understand the geological characteristics, intrusion age and petrogenetic environment, we have studied the geology, geochemistry and geochronology of intermediate granite rocks from the area. LA-ICP-MS zircon U-Pb dating shows that the granitoids were emplaced in the Early Cretaceous, from (129.3±0.8) Ma to (130.5±0.9) Ma.Geochemical analyses show that the granitoids are high in SiO2(73.19%-76.7%), alkali(K2O+Na2O=7.81%-8.41%), with A/CNK=0.93 to 1.12, displaying strong peraluminous characteristics. The rocks have low CaO(0.32%-7.31%) and MgO (0.01%-1.76%), and distinct negative Eu anomalies (δEu=0.11-1.25). Primitive-mantle normalized multi-element spider diagram displays apparent enrichments in Rb, Th and Nd, and marked depletions in Nb, Sr, P, Ti and K.These intermediate granitoids show continental collision geochemical affinities. Considering the regional tectonic setting and published information, we infer that the granites at Qieqiong were formed in the a post-collisionalsetting, when crustal thickening and delamination occurred. The magmas were sourced by basaltic magma underplating and the subsequent partial melting of the middle-lower crust.

Key words: zircon U-Pb age, whole-rock geochemistry, granite, Gangdise, tectonic setting

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