姚国龙,马向军.山东省栖霞苏家店金矿床地质特征及矿床成因[J].地质找矿论丛,1998,(4):28-37
山东省栖霞苏家店金矿床地质特征及矿床成因
GEOLOGICAL FEATURES AND GENESIS OF SUJIADIAN AU ORE DEPOSIT IN QIXIA COUNTY,SHANDONG
投稿时间:1998-10-06  修订日期:1998-10-08
DOI:10.6053/j.issn.1001-1412.1998.4. 003
中文关键词:  地质特征  矿床成因  岩浆热液  苏家店金矿
英文关键词:Geological feature  magmatic hydrothermal fluid  Shujiadian Au deposit
基金项目:
作者单位
姚国龙 冶金部天津地质研究院, 天津, 300061 
马向军 洛阳水资源设计勘查院, 洛阳, 471000 
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中文摘要:
      苏家店金矿产于玲珑花岗岩中,受北东向和北东东向断裂控制,通过对苏家店金矿地质特征、矿物组成、稳定同位素、包裹体地球化学特征等研究表明,苏家店金矿是与玲珑花岗岩有关的热液型金矿床。
英文摘要:
      Shujiadian Au deposit is located in Jiaobei terrain.Its wall rock is Linglong granite.Pb,S,O isotpe is similar to Jiaodong Group metamorphic rock,Linglong granite and Shujiadian Au deposit imply the genetic relation to the three kinds of rocks.The δ18O and δD value indicates that ore forming fluid is mainly derived from magmatic fluid,as well as mixing with a part of meteroic water in later stage.According to the above research,Shujiadian Au deposit is an anatectic magmatic deposit.
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