The study of fluid inclusions in sphalerites and associated gangue minerals (quartz, celestite, calcite and gypsum) shows that homogenization temperatures cluster around 110-150℃, with salinities of 1.6-18.0 wt% NaCl equivalent. The fluid temperature increased with the decrease in salinities during the main ore stages, and there is also a systematic westward decrease in temperature and increase in salinity in the Jinding ore district.

閃鋅礦及相關脈石礦物（石英、天青石日韩在线精品福利网页观看视频、方解石日韩免费爱插摸视频、石膏）中流體包裹體觀測的均一溫度主體在110~150℃wwwww在线国产，鹽度在1.6%~18.0% NaCl黄色网站视频无码；在時間上www.青草草，大規(guī)模成礦主要階段伴隨著流體溫度的不斷升高和鹽度的逐漸降低；在空間上又黄又硬又爽又舒服视频，金頂?shù)V區(qū)空間上從東到西自拍偷拍激情网站，成礦流體溫度明顯降低，鹽度系統(tǒng)性升高九九热这里只有精品6666。

In resent years small Fe-Cu ore bodies have been discovered at shallow depth of Zhouzhuang fluorite ore district with the associated relatively concentrated molybdenite bands.

近年來102av视频在线，在河南確山周莊螢石礦區(qū)的淺部發(fā)現(xiàn)了鐵銅小礦體，局部見及品位較高的輝鉬礦條玖玖网在线。

This paper studies the geological and geochemical characteristics of spilite-quartz keratophyre formation, and the ore-forming process in Dapingzhang ore district, Yunnan province.

本文對大平掌礦區(qū)細碧巖-石英角斑巖建造的地質地球化學特征和礦床的成礦作用進行了較為全面而深入的研究热热热热热热热热热热热热色色色色色色。