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北祁连浪力克地区毛藏花岗闪长岩年代学、Hf同位素及地球化学特征

白赟 郭周平 赵辛敏

矿床地质2017,Vol.36Issue(1):158-170,13.
矿床地质2017,Vol.36Issue(1):158-170,13.DOI:10.16111/j.0258-7106.2017.01.010

北祁连浪力克地区毛藏花岗闪长岩年代学、Hf同位素及地球化学特征

Geochronology, Hf isotopic and geochemical characteristics of Maozang granodiorite in Langlike area, North Qilian Mountain

白赟 1郭周平 2赵辛敏2

作者信息

  • 1. 核工业西藏地质调查院,四川成都610052
  • 2. 中国地质调查局西安地质调查中心,陕西西安710054
  • 折叠

摘要

Abstract

The granodiorite pluton in Langlike area of Menyuan,Qinghai,is located in the eastern Lenglongling of North Qilian Mountain.The authors conducted a study of chronology and geochemistry to constrain its geochronology and petrogenesis.Zircon LA-ICP-MS dating yielded a concordant age of (471.9 ± 8.6)Ma (MSWD=1.6),suggesting Ordovician in Early Paleozoic.Zircon Hf isotope analysis suggests that the calc-alkaline units have TDM2 values between 1112.4 and 2284.7 Ma,with εHf(t) values from-13.3 to 5.26,indicating that the magma sources were involved in crust-mantle mixing,the source region of the crust type was likely to be ancient crustal rocks of Paleoproterozoic and Mesoproterozoic.In addition,rock geochemistry indicates that the rock is a weak peraluminous potassium calc-alkaline series of Ⅰ-type granites,obviously enriched in LILE (such as K,Ba,Rb) and incompatible elements such as Th and U,and relatively depleted in high field strength elements such as Nb,Ta,Ti and P,implying a volcanic arc granite formed in a subduction environment.

关键词

地球化学/中钾钙碱性侵入岩/岩石成因/锆石U-Pb年龄/北祁连毛藏

Key words

geochemistry/potassium calc-alkaline intrusive rock/petrogenesis/zircon U-Pb age/Maozang area of North Qilian Mountain

分类

天文与地球科学

引用本文复制引用

白赟,郭周平,赵辛敏..北祁连浪力克地区毛藏花岗闪长岩年代学、Hf同位素及地球化学特征[J].矿床地质,2017,36(1):158-170,13.

基金项目

本文受中国地质调查局“青海门源县银灿-浪力克1∶5万成矿预测”项目(编号:1212011221043)和“青海门源县宁缠河-牛头山一带铜多金属矿调查评价”项目(编号:12120115022401)资助 (编号:1212011221043)

矿床地质

OA北大核心CSCDCSTPCD

0258-7106

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