毛光武,曹亮,严卸平,舒文辉,祖俊龙,王波涛.浅成低温热液型金矿研究综述[J].地质找矿论丛,2015,30(1):121-132
浅成低温热液型金矿研究综述
A review of research on epithermal gold deposits
投稿时间:2014-09-29  
DOI:10.6053/j.issn.1001-1412.2015.01.018
中文关键词:  浅成低温热液金矿床  构造-岩浆背景  成矿机理  成因模式  找矿标志
英文关键词:epithermal gold deposits  tectonomagmatism  metallogenic mechanism  genetic model  prospecting criteria
基金项目:
作者单位
毛光武 中国地质大学(武汉), 武汉 430074
中国冶金地质总局二局, 福州 350001 
曹亮 中国地质大学(武汉), 武汉 430074 
严卸平 中国冶金地质总局二局, 福州 350001 
舒文辉 中国冶金地质总局二局, 福州 350001 
祖俊龙 中国冶金地质总局二局, 福州 350001 
王波涛 中国冶金地质总局二局, 福州 350001 
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中文摘要:
      浅成低温热液型金矿是重要的金矿类型,近年来对该类矿床的地球化学特征、成矿岩浆背景、成矿机理及成矿模式等方面的研究取得了重大进展。研究表明,该类矿床形成时代主要是中、新生代,其次为晚古生代;高硫化型矿床主要形成于挤压应力场环境和流体混合导致成矿物质沉淀, 而低硫化型矿床主要产于张性或中性环境下由于流体的沸腾使得成矿物质沉淀;蒸气冷却收缩模式合理地解释了浅成低温热液矿床和斑岩矿床在时间和空间上的共生关系,对指导找矿具有一定的实践意义。
英文摘要:
      The epithermal gold deposit is one of the most important types of gold deposit. Significant advances have been made in the latest decades, including the geochemical characteristics, the relationship with intrusive rocks, the metallogenesis and metallogenic model. The researches indicate that this type of deposit is mainly formed in Mesozoic and Cenozoic. Next to the two eras is Late Paleozoic. The high sulphidation gold deposit is mainly resulted from the fluid mixing under the compressional stress regime while the low sulphidation gold deposit from the boiling under the extensional stress regime. Cooling and contracting model can explain reasonably the temporal and spatial association of the epithermal Au deposit and porphyry copper-gold deposit thus is of guiding significance for future prospecting.
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