2) polygenetic U-Mo deposit
复成因铀钼矿床
1.
The deposit is a polygenetic U-Mo deposit produced by post-hydrothermal molybdenum-bearing superimposition on the basis of post-magmatic hydrothermal uranium mineralization in Early Yanshanian.
该矿床是在燕山早期岩浆期后热液铀矿化的基础上,经后期含钼热液叠加作用而形成的复成因铀钼矿床。
3) polygenetic compound deposit
多因复成矿床
1.
Based on the basic theory and method o f"polygenetic compound deposit",this article analysed geological mineralization characteristics and metallogenic law of the3110uranium deposit.
本文运用“多因复成矿床”的基本理论和方法,对华南3110铀矿床的地质矿化特点及其成矿规律进行了深入的解剖。
2.
Polygenetic compound deposit is characterized by “ five many” .
作者于1979年开始提出多因复成矿床概念的主旨，是为了阐明从时空四维并重的角度来认识与研究成矿的重要性。
4) polygenetic corn pound gold ore deposit
多因复成金矿床
5) Genetic model of uranium deposit
铀矿床成因类型
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：配成复混肥料(见复混肥料)
配成复混肥料(见复混肥料)
肥料。配成复混肥料见复混
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