公郎 meaning in English
gonglang
kimiro
Examples
- The pressure of mineralization is in a range from 100 mpa to 225 mpa , the corresponding temperatures of mineralization are about 317 - 346c , and the depths of mineralization are about 3 . 51 - 7 . 89 km
公郎弧成矿流体系统成矿压力大约为100 225mpa ，成矿温度为317 346 ，成矿深度约为3 . 51 7 . 89km 。 - The zijinshan fluid system and the gonglang fluid system were driven by the stress of extrusion nappe onto the basin and the thermal driving force of magmatism . when the fluids cycling in the basin encountered the boundary of reduction - oxidation or underwent fluid mixing , phase separating and fluid boiling caused by fault - induced pressure reducing , the physical chemistry condition abruptly changed and mineralization then took place
在盆地两侧挤压推覆构造应力及岩浆作用热力驱动下，紫金山背斜和公郎弧两大流体系统的流体在盆地中运动，当遇到氧化还原界面或遭受流体混合、相分离及断裂导致的减压沸腾时，因物理化学条件发生重大变化而导致成矿作用的发生。 - Based on the studies of microthermometry , gas composition , liquid composition , rare earth elements , ore - forming elements and 13c , d , 18o of fluid inclusions from the mineralization district and the representative deposits , such as zacun gold deposit , shuixie copper - cobalt deposit , shiyancun stibium deposit and bijiashan stibium deposit , two metallogenic fluid systems have been distinguished , i . e . , zijinshan metallogenic fluid system and gonglang metallogenic fluid system in weishan - yongping mineralization district
矿化集中区及扎村金矿、水泄铜钴矿、石岩村锑矿、笔架山锑矿等典型矿床流体包裹体的显微测温、气相成分、液相成分、稀土元素、重金属元素及~ ( 13 ) c ， d ， ~ ( 18 ) o稳定同位素的研究表明，云南巍山-永平地区铜金多金属矿化集中区存在两个成矿流体系统：紫金山背斜成矿流体系统与公郎弧成矿流体系统。 - The author suggests that the three lithosphere - scale faults , lancangjiang fault , jinshanjiang - ailaoshan fault and axis fault in the middle of the basin , are the main geological structures that control the formation of basin , magmatism and metallogenic congregate district . the anticline structure with an axis of triassic strata and the related fault system within the basin , and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields . junctions of two or more faults with different orientation , interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies
认为澜沧江断裂、金沙江-哀牢山断裂及盆地中轴断裂这三条岩石圈断裂是主要的控盆-控岩(岩浆岩)构造及矿集区尺度的控矿构造；盆地中以三叠系为轴的背斜构造及相关的断裂系统、盆地西南缘公郎弧形构造等是矿田尺度的控矿构造；多组断裂的交叉、层间破碎带及地层柱中的氧化还原界面是形成矿体的有利部位。