| 释义 |
Hongtoushan
基本例句
红透山¹⁰⁰
Brought up the new path for safety and validity to use mid deep hole mine method in Fushun Hongtoushan Copper Mine.为红透山铜矿中深孔采矿方法的安全、高效使用提出了新的途径。
The Hongtoushan copper-zinc deposit was formed in submarine volcanic eruptional-sedimentary environment in Archean intracratonic rift trough.红透山式铜-锌矿床形成于太古代克拉通裂谷槽盆中海底火山喷发-沉积环境。
Massive sulfide Cu-Zn deposit of Hongtoushan type which occurs in Archeozoic granitic greenstone terrain in Qinyuan area of Liaoning possesses unique geochemical characteristics.产于辽宁省清原地区太古宙花岗-绿岩地体中的红透山式块状硫化物铜锌矿床,具有独特的地球化学特征。
The post metallogenic metamorphism of Hongtoushan Archean Cu-Zn massive sulphide deposit, Liaoning Province of NE China, belongs to upper amphibolite facies with three phases of deformations.辽宁红透山铜-锌块状硫化物产在太古宙绿岩带中,矿床形成后经历了强烈的变形和变质,变质程度达高级角闪岩相。
The “Hongtoushan type” of copper deposits in Fushun, Liaoning Province, occurred in Hunbei Archean greenstone belt, is macroscopically controlled by the Hongtoushan greenstone formation.摘要辽宁抚顺“红透山式”铜矿产在浑北太古宙绿岩带内，宏观上受控于太古宙红透山岩组绿岩建造。 |