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1)  The deep origin of ore forming
深源成矿论
1.
The deep origin of ore forming is a new theory for prospcting in situ leachable sandstone type uranium.
深源成矿论是可地浸砂岩型铀矿地质找矿的一种新思路 ,在松辽盆地南部铀矿勘查中得到了较好的应用。
2)  deep origin metallogenesis
深源成矿
1.
Based on summarizing the geological background of Lujing uranium ore~field,it is analyzed that deep origin metallogenesis,deep~seated strike~slip faults,thermal metamorphic belt and granite~porphyry play important roles in uranium mineralizatiom.
在综述鹿井铀矿田地质背景的基础上,重点分析了深源成矿、深大走滑断裂、热变质带、花岗斑岩对铀成矿的重要作用。
3)  juvenile fluid mineralization
深源流体成矿
4)  deep origin mineralization fluid
深源成矿流体
5)  metallogenic depth
成矿深度
6)  mineralization depth
成矿深度
1.
According to the study of quantitative statistics model,we find that the mesogenic vein type gold deposits which formed in compressional geodynamic enviroment have relatively deep mineralization depth,large scale and strong mineralization;whereas the epigenic vein type gold deposits which formed in tensional geodynamic enviroment have relatively shallow mineralization depth,small scale .
定量统计模型研究发现 ,形成于挤压地球动力学环境的中深成脉型金矿 ,成矿深度相对深 ,规模大 ,矿化强 ;形成于拉张地球动力学环境的浅成脉型金矿 ,成矿深度相对浅 ,规模小 ,矿化
2.
From the model of mineralization depth, theoretical mineralization depth of the two types can be got, from 2.
本文以成矿深度作为脉型金矿的分类依据,胶东地区可分为中深和浅成两类脉型金矿。
补充资料:成业论
【成业论】
 (书名)大乘成业论之略名。
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