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热液石英中微量元素特征及应用:认识与进展

陈小丹 陈振宇 程彦博 叶会寿 汪欢

地质论评2011,Vol.57Issue(5):707-717,11.
地质论评2011,Vol.57Issue(5):707-717,11.

热液石英中微量元素特征及应用:认识与进展

Distribution and Application of Trace Elements in Hydrothermal Quartz:Understanding and prospecting

陈小丹 1陈振宇 2程彦博 1叶会寿 2汪欢1

作者信息

  • 1. 中国地质大学(北京)地球科学与资源学院,北京,100083
  • 2. 中国地质科学院矿产资源研究所,北京,100037
  • 折叠

摘要

Abstract

Based on chemical properties and crystal structure characteristics of quartz, together with the acquired cogination and achievement of this field all over the world, the writers want to give a review on the distribution and application of trace-elements in hydrothermal quartz. There are three main substitution modes govern the incorporation of structural trace elements; single substitution, double substitution, compensated. As the intensity of SEM-CL image is related to trace-elements content in quartz, trace-elements in quartz can be applied to constrain geologic process. According to the distribution of trace-elements in quartz formed at different temperature in hydrothermal deposits, the metallogenetic temperature can be appromately judged, and be mensurable by TITANiQ. The composition and distribution of trace-elements in quartz can tell quartz in magmatic stage from hydrothermal stage, and the phase of hydrothermal quartz can be effectively distinguished as well. Aluminum and titanium concentration in quartz is strongly dependent on pH of hydrothermal fluids, which can be used to detect pH of quartz precipitation and speculate the evolution of hydrothermal fluids.

关键词

石英/微量元素/阴极发光/热液演化/综述

Key words

quartz/ trace elements/ cathodoluminescence/ hydrothmal evolution/ review

引用本文复制引用

陈小丹,陈振宇,程彦博,叶会寿,汪欢..热液石英中微量元素特征及应用:认识与进展[J].地质论评,2011,57(5):707-717,11.

基金项目

本文为全国危机矿山接替资源找矿项目(编号20089949和200841019)的成果. (编号20089949和200841019)

地质论评

OA北大核心CSCDCSTPCD

0371-5736

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