王银宏.铜陵天马山金硫矿床成矿系统研究[J].地质找矿论丛,2005,(2):106-110
铜陵天马山金硫矿床成矿系统研究
A STUDY ON THE METALLOGENIC SYSTEM OF TIANMASHAN GOLD-SULFUR DEPOSIT IN TONGLING
投稿时间:2004-05-26  
DOI:10.6053/j.issn.1001-1412.2005.2. 006
中文关键词:  成矿系统  天马山金硫矿床  铜陵
英文关键词:Metallogenic system  Tianmashan Gold-Sulfur deposit  Tongling city
基金项目:国家973项目(NO1.G1999043215);中美矿产资源评价合作研究项目联合资助。
作者单位
王银宏 中国地质大学, 北京, 100083 
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中文摘要:
      天马山金硫矿床位于铜官山背斜近倾没端、靠近轴部的东南翼,天鹅抱蛋山岩体东侧。文章从成矿系统的角度对区内多金属矿床进行了阐述:①矿区成矿系统要素,如矿源场、成矿流体、成矿能量和储矿场;②成矿流体在流体输运化学反应耦合成矿作用过程中,与成矿流体组分相关的成分守恒方程;③在特定的时空条件下,矿区矿源场、流体场和能量场的耦合过程;④成矿作用机理。
英文摘要:
      The Tianmashan Gold-sulfur deposit is located nearly to the pitching end of Tongguanshan anticline, southeast side of its axis, and east of the Tian'ebaodanshan intrusion. Based on the former research, authors depend on metallogenic system theory to study this polymetallic deposit. the system includes: factors, such as the ore-source field, the ore-forming fluid, the ore-forming energy, and the ore storing field, the component conservation equation relative to the ore-forming fluid components during the coupled ore-forming processes of fluid transport-chemical reactions, the coupled processes of the ore source field, fluid field, and energy field under the spacial time-space condition, and the ore-forming mechanism.
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