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1)  mineralization breadth
成矿广度
2)  metallogenic depth
成矿深度
3)  ore-forming temperature
成矿温度
1.
In order to understand the ore-forming temperature and source materials,this paper studied fluid inclusions well developed within calcite and quartz from both alteration type and quartz vein type gold deposits in the central part of the Yi-Shu fault belt.
为探讨沂沭断裂带中段地区金矿的成矿温度和物质来源,对蚀变岩型和石英脉型金矿内方解石、石英中流体包裹体的研究表明,这2类金矿中流体包裹体较为发育,有单一液相包裹体、气液两相包裹体和富气相包裹体等3种类型;其冰点温度为-2~-8。
4)  metallogenic temperature
成矿温度
1.
The metallogenic temperatures vary for different genetic types of deposits.
不同成因类型矿床成矿温度亦有差异 ,“斑岩型”属中高温矿床 ,“火山热液型”属中低温矿床 ,“新类型”金矿床和“浅成低温热液型”金矿应属低温热液矿床 。
2.
The metallogenic temperature of Jinya gold deposit in Guangxi province has been analysed by way of infrared spectroscopic method in the paper, which is 255-300℃.
本文用干酪根的红外光谱方法,分析了广西金牙金矿的成矿温度为255—300℃。
5)  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。
6)  Linglong-Jiaojia style gold deposit
成矿深度
1.
The depths for the formation of typical Linglong-Jiaojia style gold deposits were estimated using the theory of influence on the hydrostatic pressure by the tectonic force and the method of tectonic correction.
应用构造作用力影响静水压力的理论,用构造校正方法,测算了玲珑-焦家式金矿的成矿深度。
补充资料:广度经济

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