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隐爆角砾岩型金矿研究述评
引用本文:卿敏,韩先菊.隐爆角砾岩型金矿研究述评[J].黄金地质,2002,8(2):1-7.
作者姓名:卿敏  韩先菊
作者单位:1. 中国地质大学,北京,100083;武警黄金地质研究所,河北,廊坊,065000
2. 武警黄金地质研究所,河北,廊坊,065000
摘    要:隐爆角砾岩型金矿是国内外一种具有重要经济价值的矿床类型。不同类型隐爆角砾岩是该类金矿最主要的容矿围岩。造成隐爆作用发生最直接的因素是受热的多源流体或气体,岩浆隐蔽爆破主要作用方式是气爆和浆爆,其次是热液注入。通常气爆发生于早期,浆爆较晚,而热液注入最晚。浅成-超浅成中酸性斑岩体是隐爆角砾岩形成的决定性因素,气液的隐蔽爆破作用是隐爆角砾岩有角砾岩型金-多金属矿床形成的原因,成岩与成矿是同一地质过程不同阶段产物。不同级别的构造对该类型金矿档的产出空间、矿化类型和矿体形态等具有分级控制作用,矿化、蚀变存在明显的垂向分带及其空间套叠。该类型金矿可划分为Au-Ag和Au-Cu系列,矿床系列、矿床规模有富矿部位可通过一系列指标进行判别。

关 键 词:金矿床  隐爆角砾岩  浅成中酸性侵入岩  成矿作用  矿化类型  地质作用
文章编号:1006-558X(2002)02-0001-07
修稿时间:2002年3月28日

A Commentary of Cryptoexplosion Breccia Type Gold Deposits
QING Min ,HAN Xian ju.A Commentary of Cryptoexplosion Breccia Type Gold Deposits[J].Gold Geology,2002,8(2):1-7.
Authors:QING Min    HAN Xian ju
Institution:QING Min 1,2,HAN Xian ju 2
Abstract:Cryptoexplosion breccia type gold deposit is one type of deposits which has great economic value in China and aboard.Different cryptoexplosion breccia is the host rock of the gold deposit. The direct reason of the cryptoexplosion is the polyphyly liquid or gas that is heated. The main magmatic cryptoexplosion is gas or magma explosion, next is hydrothermal. Usually gas explosion occuered in early period, next is magma explosion and hydrotnermal is the latest. Hypabyssal superhypabyssal intermediate acidic intrusive rocks is the determinative factor of the former of cryptoexplosion breccia.The cryptoexplosion of gas and liquid is internal cause of cryptoexplosion breccia type and breccia type gold polymetallic deposits, lithogenesis and mineralization were the products of the same geological process of different stage. Different class structure controlled the space of gold deposit output,types of mineralization and ore pattern, mineralization and alteralition had obvious vertical zoning and telescoping in space. This type of gold deposit can be divided into Au Ag and Au Cu series, the deposit series, the scale of deposit and gold rich position can be judged by series quota.
Keywords:gold deposit  cryptoexplosion breccia  intermediate acidic intrusive rocks
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