1) mining area temperature
矿区温度
2) 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。
3) 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℃。
4) semi_melting temperature
熔矿温度
5) mine tmperature
矿井温度
6) humidity of mining area
矿区湿度
补充资料：铂电阻温度表(见电阻温度表)
铂电阻温度表(见电阻温度表)
表。bod旧nZu wendubiao铂电阻温度表见电阻温
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条