矿床成因类型 meaning in Chinese
genetic type of ore deposit
genetictypeoforedeposit
Examples
- The minerogenic types of nonmetallic deposits related to cenozoic basalts and their minerogenic mechanism
与新生代玄武岩有关的非金属矿床成因类型及成因机理探讨 - The study of the regional geological setting , occurence mode of ore body , ore rocks , and orecontrolling factors of shiyintan gold deposit indicates that it is an epithermal volcanic hydrothermal gold deposit
摘要通过对石英滩金矿床区域地质背景、矿体产出形态、矿石特征、成矿控制因素的研究，认为矿床成因类型应属浅成低温火山热液型金矿床。 - A comprehensive study has been carried out on the regional geology , mining area geology and ore - deposit geology combined with isotope geology , metallogenic conditions , mineralization regularities and genetic types of the ore deposit in this paper
本文就该矿床区域地质、矿区地质、矿床地质及矿床的同位素地质学、成矿条件和矿化规律、矿床成因类型等进行了阐述和讨论。 - The ore - forming material is mostly from volcanic rock , and sub volcanic rock provides the main thermal and some mineral materials . the ore - forming fluid is from meteoric water . as a result , it should be a kind of adularia - sericite type of epithermal gold deposit
成矿物质主要来自矿区火山岩围岩，次火山岩提供了主要热源和部分矿源，成矿流体来自大气降水，矿床成因类型为低硫化物冰长石?绢云母型浅成低温热液型金矿。 - The mineralizing fluid in lanping - baiyangping area is deep circulatory thermal brine as a whole , the mineralizing matter mainly comes from deep , and the genetic type of the deposit belongs to the low - to - moderate - temperature hydrothermal silver polymetallic ore deposit related to nappe structures
因此，兰坪白秧坪地区成矿流体总体为深部循环的热卤水溶液，成矿物质主要来源于深部，矿床成因类型属于与推覆构造有关的中低温热液银多金属矿床。