1)  host rock
容矿层
1.
The paper deals with the cover rock lithology-the host rock structure combination control on ore fluid in Jinlongshan Au deposit.
以金龙山—丘岭金矿床为例,通过对发育在容矿层上的构造类型与其上封盖层岩性类型进行研究,划分出9种构造与盖层岩性组合类型,并分析其对含金热液的控制,总结出中-低温热液卡林型金矿床富集规律:Ⅰ型组合发育区容矿层的含矿液性最好;Ⅲ,Ⅵ,Ⅸ型组合发育区容矿层的含矿液性最差;Ⅱ,Ⅳ,Ⅴ,Ⅶ,Ⅷ组合发育区容矿层含矿液性较好。
2)  host position
容矿层位
1.
On the basis of the metallogenic characteristi cs of the Au deposit in the southern part of Tonghua area, the host position, wall -rock alteration and ore-control structure were analyzed.
本文通过分析通化南部金矿成矿特点,并把容矿层位、围岩蚀变、控矿构造作为在通化南部寻找金矿的三要素。
3)  ore-containing
容矿
1.
After the main active stage of the rift, a series of tectonics, consisted of prin-cipal faults, secondary faults and fractures were induced and play a role as ore-transmittingand ore-containing in the formation of the gold deposit.
滩间山金矿产于柴北缘裂谷西段的裂肩部位,在裂谷活动期后余动下,引生了主干断裂、次级断裂、裂隙的配置构造系列,为金矿的形成起到了导矿、容矿作用。
4)  ore-held fissure
容矿裂隙
5)  host rock
容矿岩石
1.
Regional deep-fault is the main pathway for meteoric water and geothermal fluids,subsidiary fracture is ore depositing structures,and fault tectonite are the main host rocks.
区域性深大断裂是沟通天水和地热流体的主要通道,次级断裂是矿体的储矿构造,脆性粗碎屑岩和火山碎屑岩(沉积火山岩)构成的断裂构造岩是主要的容矿岩石。
6)  host strata
容矿地层
参考词条
补充资料:等容热容
分子式:
CAS号:

性质:系统在体积不能改变的条件下温度升高1K所需的热,符号Cv。此时系统所吸取的热完全用来增加其内能。因为等容过程中系统吸热Qv=△U,所以Cv就是系统升高1K时其内能的变化。用数学式表示,为 Cv=其中代表偏微分,下脚V表示体积不变。关于Cv与Cp关系参见等压热容。

说明:补充资料仅用于学习参考,请勿用于其它任何用途。