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对河台金矿成矿作用的新构想
引用本文:窦海清,冷慧娟.对河台金矿成矿作用的新构想[J].华南地质与矿产,2007(3):49-55.
作者姓名:窦海清  冷慧娟
作者单位:广东省地质勘查局七一九地质大队,广东,肇庆,526020
摘    要:通过分析区域成矿作用背景及河台地区加里东-燕山期成矿物质活化、迁移、富集、沉淀条件,认为燕山期华南地幔柱活动对河台金矿的形成起到关键作用,深源流体携带的大量成矿物质是金的主要来源,地幔柱构造、深大断裂、深部构造及韧性剪切带-韧脆性构造构成了完善的金的运移和再富集成矿体系。河台地区在燕山期具备了发生大规模成矿作用的主要条件。

关 键 词:成矿作用  成矿背景  地幔柱  成矿物质  含矿流体  燕山期  河台金矿
文章编号:1007-3701(2007)03-0049-07
修稿时间:2007-04-18

New Thoughts about Ore-Forming Process of Hetai Gold Deposit
DOU Hai-qing,LENG Hui-juan.New Thoughts about Ore-Forming Process of Hetai Gold Deposit[J].Geology and Mineral Resources of South China,2007(3):49-55.
Authors:DOU Hai-qing  LENG Hui-juan
Institution:No. 719 Geological Team, Guangdong Bureau of Geology Exploration, Zhaoqing 526020, Guangdong, China
Abstract:Based on the analysis of the regional deposit-forming background and the conditions of activation,migration,enrichment and precipitation of ore-forming materials in Hetai area from Caledonian to Yanshanian period,believe that the pulsation and upwelling of the mantle plume in late Yanshanian period in South China plays a keywords on formation of Hetai gold deposit.mass of ore-forming materials caarried by deeply-derived fluid is major source of gold.Mantle plume tectonics,deep big fault belt,deep structure and ductile shear zone,ductile-brittle structure composition perfect migration,enrichment once more and metallogenic system of gold.Hetai area possessed main geological condition that took place large scale mineralization in the Yanshanian period.
Keywords:mineralization  deposit-forming background  mantle plume  ore-forming materials  the metallogenic fluids  Yanshanian period  Hetai gold deposit
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