1) crust-mantle metallogeny
壳幔成矿
2) crust_mantle metallogeny
壳幔成矿学
1.
The research of crust_mantle metallogeny through connecting the mineralization with the deep process has become an important trend of regional metallogeny.
壳幔成矿学是联结深部地质学与区域成矿学的重要桥梁。
3) crust-mantle boundary metallogenesis
壳幔界面成矿
4) crust mantle mineralization
壳幔成矿作用
5) crust-mantle superimposed reforming mineralization
壳幔叠加成矿
6) mantle crust polygenetic compound deposit
幔-壳型多因复成矿床
1.
According to the research of strata element contents, REE, stable isotope and wall rock alterations, ore forming substances are from both mantle and crust, and the ore deposit has the characteristics of mutiple metallogenesis and polygenetics, belonging to mantle crust polygenetic compound deposit.
对矿区地层元素丰度、稀土元素、稳定同位素及围岩蚀变等进行研究，结果表明，成矿物质有幔、壳两大来源，矿床具多期多成因的特征，属幔－壳型多因复成矿
补充资料：朱幔
1.红色的帷幕。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条