山东夏甸金矿幔源流体初探
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引用本文:张群喜,孙忠实.2003.山东夏甸金矿幔源流体初探[J].地球学报,24(2):127-131.
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作者单位
张群喜 吉林大学地球科学学院吉林长春130026 
孙忠实 吉林大学地球科学学院吉林长春130026 
基金项目:国家自然科学基金项目(编号:40272051,40172036)
中文摘要:山东夏甸金矿矿床成因一直有变质热液、岩浆热液和天水之争。经过工作得知,还有幔源流体加入成矿,其主要证据有:①招平深大断裂带存在,为幔源流体加入成矿提供了通道;②金矿脉与中基性脉岩相互交切、相伴产生;③S、H、O、C等同位素测定值表明,含金流体主要来自幔源。
中文关键词:金矿  幔源流体  中基性脉岩  夏甸
 
A Tentative Discussion on Mantle Fluids in the Xiadian Gold Deposit, Shandong Province
Abstract:There has been long controversy on the genesis of the Xiadian gold deposit. Some hold that it is of metamorphic hydrothermal origin, others argue for magmatic hydrothermal genesis, and still others think that it results from ground water.Nevertheless,further work shows that the mantle fluids might have played an important role in the formation of the deposit. The main evidence is:①the Xiadian gold deposit is located in the Zhaoping deep fault;②the gold veins are usually associated with the intermediate basic rock veins;③the estimated S,H,O and C isotopic values indicate that gold bearing fluids mainly came from the mantle fluids.
keywords:gold ore deposit  mantle fluids  intermediate-basic rock veins  Xiadian
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