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论华夏成矿省

杨明桂 陈祥云 吴俊华 衷存堤 王岩

地质论评2024,Vol.70Issue(3):823-838,16.
地质论评2024,Vol.70Issue(3):823-838,16.DOI:10.16509/j.georeview.2024.04.061

论华夏成矿省

Discussion on Cathaysian Metallogenic Province

杨明桂 1陈祥云 1吴俊华 1衷存堤 2王岩3

作者信息

  • 1. 江西省地质局,南昌,330036
  • 2. 江西省地质调查勘查院基础地质调查所,南昌,330030
  • 3. 中国地质科学院矿产资源研究所,自然资源部成矿作用与资源评价重点实验室,北京,100037
  • 折叠

摘要

Abstract

This paper gives a brief discussion on the Cathaysian Metallogenic Province with strategic mineral resources holding an important position,which was definited in the monograph of the"Mineral Geology of China:Tectonic Evolution and Mineralization in South China Ocean—Marginal Pacific Ocean"(2020):① The Cathaysian Metallogenic Province is located in an extensive composite zone between the Paleo-South China Ocean Metallogenic Domain and the Marginal Pacific Metallogenic Domain,which underwent the development and evolution of the Early-Craton→South China Ocean rift system→epicontinental sea→continent since the Early Precambrian.Furthermore,it was subjected to multiphase orogeny,especially the extremely extensive Yanshanian intracontinental activation orogeny,being the world-class tungsten geochemical block,which forms the superior metallogenic genetics.② Major metallogenic characteristics:including South China Ocean and it's metallogenic of marginal arc depression remnant,and the large-scale sedimentary metallogenitc during the Nanhua interglacial period and post-glacial period;multiphase and large-scale S-type magmatic metallogenic was predominated by the tungsten,secondly,nonferrous metal,uranium,precious metals and non-metallic;I-types magmatic mineralization is dominated by copper,with iron,nonferrous metals and precious metals,as well as the super-large ore concentrated group along the Qinzhou—Hangzhou metallogenic belt,which has become an"eye"for prospecting in the"deepth",etc.③ During the Yanshanian Movement,the magmatic and metallogenic"core—mantle"type spacial—temporal evolution regularity,as well as multi-system composite tectonic framework present the dynamic system,mainly due to the left-lateral shear between the continent and ocean with combination of ocean subduction,intracontinental multidirection convergence and crustal creep effect.

关键词

华夏成矿省/成矿基因/成矿特征/燕山运动/成岩成矿动力机制

Key words

Cathaysian Metallogenic Province/metallogenic genetics/metallogenic characteristics/Yanshanian Movement/diagenetic and metallogenitc dynamic mechanism

引用本文复制引用

杨明桂,陈祥云,吴俊华,衷存堤,王岩..论华夏成矿省[J].地质论评,2024,70(3):823-838,16.

基金项目

本文为中国地质调查局"中国矿产地质志"项目(编号:DD20221695、DD20190379),委托"华南洋—滨太平洋构造演化与成矿"研究专题项目(编号:矿调合同[2017]第83号)的成果. This paper is supported by the Geological Survey Project of"Annals of Geology of Mineral Resources of China"(Nos.DD20221695,DD20190379),the Tectonic Evolution and Mineralization in South China Ocean-Marginal Pacific Ocean(Mining Regulation Contract[2017]No.83)which is commissioned by Institute of Mineral Resources,Chinese Academy of Geological Sciences.This English abstract is reviewed by Longmei Librarian.We would like to express our deep gratitude (编号:DD20221695、DD20190379)

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