摘要
东山钨矿床产于尖峰岭花岗岩体与泥盆系和石炭系石灰岩的接触带中,钨矿体的形成与接触带构造及古岩溶的发育程度密切相关,矿床成因为夕卡岩 热液充填交代型白钨矿床。采用地质与物化探结合的方法,进行了成矿预测,圈定了找矿远景区。
Dongshan scheelite deposit is of skarn-hydrothermal fluid replacement scheelite deposit and its formation is closely related to the development degree of structure and fossil karsk at the contact zone. The authors integrate geological, geophysical and geochemical data to make metallogenic prognosis and outline the prospects in the mine area.
出处
《地质找矿论丛》
CAS
CSCD
2004年第1期13-16,共4页
Contributions to Geology and Mineral Resources Research
关键词
东山钨矿
夕卡岩-热液充填交代型矿床
成矿预测
湖南省
scheelite
skam-hydrothermal metasomatic filled replacement deposit
metallogenic prognosis
Dongshan, Hunan province
