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豫西崤山东部中河岩体锆石U-Pb年龄、地球化学和Lu-Hf同位素特征

肖建辉 武广 孟宪锋 范海洋 李铁刚 田强国 徐文超

矿床地质2018,Vol.37Issue(2):290-310,21.
矿床地质2018,Vol.37Issue(2):290-310,21.DOI:10.16111/j.0258-7106.2018.02.005

豫西崤山东部中河岩体锆石U-Pb年龄、地球化学和Lu-Hf同位素特征

Zircon U-Pb age, geochemistry and Lu-Hf isotopic characteristics of Zhonghe intrusion in eastern Xiaoshan, Henan Province

肖建辉 1武广 2孟宪锋 3范海洋 1李铁刚 2田强国 3徐文超3

作者信息

  • 1. 河南省地质矿产勘查开发局第一地质矿产调查院,河南 洛阳 471000
  • 2. 河南省金银多金属成矿系列与深部预测重点实验室,河南 洛阳 471000
  • 3. 中国地质科学院矿产资源研究所 国土资源部成矿作用与资源评价重点实验室,北京 100037
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摘要

Abstract

The granitic Zhonghe intrusion;located in eastern Xiaoshan of Henan Province;has a close genetic relationwith the large-sized Zhonghe Ag-Pb-Zn deposit recently discovered in Luoning County.Two granite porphyry samples from the Zhonghe intrusion were selected for LA-ICP-MS zircon U-Pb dating,which yielded weighted mean 206pb/238U ages of (129 ± 0.7) Ma (MSWD =0.78) and (131 ± 1.5) Ma (MSWD =1.70),respectively,indicating that the Zhonghe intrusion formed during Early Cretaceous.The petrogeochemical data show that Zhonghe intrusion has high w(SiO2) and w(K2O) content and low w(Na2O) content,its A/CNK values vary from 1.03 to 1.63,and its Mg# values range from 25 to 50.The Zhonghe intrusion generally belongs to a high-K calk-alkaline series.The granitic rocks reveal low w(Yb) content and intermediately-weakly negative Eu anomalies,and their rare earth element (REE) distribution patterns are characterized by enrichment of light REEs (LREEs),with strong LREEs fractionation but weak heavy REEs (HREEs) fractionation.The Zhonghe intrusion has low Sr and Y content,and is characterized by enrichment of Rb,Ba,U,K and LREEs and depletion of Nb,Ta,P,Zr,Hf,Ti and HREEs.The granite porphyry has low zircon εHf(t) values of-34.4 ~-23.2 with an average value of-26.9,and old Hf two-stage model ages of 2485 ~ 3182 Ma with an average age of 2714 Ma.The petrogeochemical characteristics and Hf isotopic compositions indicate that magmatic source of the Zhonghe intrusion was dominated by a Neoarchean crust with the addition of a small amount of Mesoarchean crust,and that the Zhonghe intrusion most likely originated from a partial melting of the Meao-Neoarchean crust,which formed in a Meao-Neoarchean island arc environment.

关键词

地球化学/锆石U-Pb年龄/Lu-Hf同位素/中河岩体/崤山/豫西

Key words

geochemistry/zircon U-Pb age/Lu-Hf isotopes/Zhonghe intrusion/Xiaoshan/western Henan Province

分类

天文与地球科学

引用本文复制引用

肖建辉,武广,孟宪锋,范海洋,李铁刚,田强国,徐文超..豫西崤山东部中河岩体锆石U-Pb年龄、地球化学和Lu-Hf同位素特征[J].矿床地质,2018,37(2):290-310,21.

基金项目

本文得到中国地质调查局地质调查项目(编号:12120114035201)和中国矿产地质与成矿规律综合集成和服务(矿产地质志)项目(编号:DD20160346)的联合资助 (编号:12120114035201)

矿床地质

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