测温学 meaning in Chinese
thermometry
Examples
- Beishan deposit which located on the most north part of yinshan deposit has an independent change trend high to low in ore - forming temperature with from east to west in pace . this indicates that quartz porphyry 5 # may be the mineralization center of beishan deposit
本文通过流体包裹体显微测温学研究得出初步结论，北山矿床成矿温度从东到西呈由高到低的变化趋势，表明北山的5 #石英斑岩是北山矿床成矿作用的中心。 - Undertaking isotopic geochronological study on ar - ar , adopted the fast - neutron activation dating technique to test 40ar - 39ar age of quartz from au - bering quartz veinlet ore in the deposit , and well - defined plateau age of 210 . 59 ma ? . 92 ma , the lowest apparent age of 208 . 07 ma ? . 22 ma , and isochron age of 207 . 14 ma ? 1 . 92 ma
通过流体包裹体显微测温学研究，表明金矿床的均一温度成矿早阶段为270 320 ，成矿主阶段为170 250 ，成矿晚阶段为110 250 ，呈逐渐降低的趋势，低温成矿作用明显。 - On the basis of this , the paper specially discusses the ore precipitating mechanism and the ore origin . fluid - inclusion observations and microthermometric data suggest that the ore - forming fluid is middle - low temperature hydrothermal solution , it also reports the presence of high - salinity inclusions containing hilite in porphyry rock and ore - hosted quartz vein
流体包裹体岩相学和显微测温学研究表明，银山矿床成矿流体属于中低温热液范畴，在石英斑岩和多金属矿脉中都发现有含石盐子矿物的高盐度流体包裹体。