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。
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 δ 18 O 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.
出处
《地质找矿论丛》
CAS
CSCD
1998年第4期28-37,共10页
Contributions to Geology and Mineral Resources Research
关键词
地质特征
矿床成因
岩浆热液
金矿床
Geological feature,magmatic hydrothermal fluid,Shujiadian Au deposit
