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- W2378171806 abstract "The Jiama copper and polymetal deposit is located in a back-arc sedimentary basin and occurs as stratiform and stratoid bodies in the transitional zone between the reef limestone(J_3d) and sandy slate(K_1l).Skarn as ore-bearing rock in the Jiama deposit,having particular geological characteristics,has been concerned greatly by investigators.On the basis of studies on the characters of the fluid inclusions in the minerals,such as homogenization temperature and composition,and compared with the fluid composition and temperature of the fluid inclusions from the Jiama skarn and typical skarn-type deposits,the hot brine in modern seafloor,this article holds that the formation temperature,fluid composition of the stratabound skarn mainerals in the Jiama deposit are different greatly from the typical skarn-type deposits,but are comparability similar to the hot brine from modern seafloor.So,the authors conclude that the stratabound skarn of the Jiama deposit has nothing to do with magma hydrothermal solution,and however,has likely something to do with the hot brine in the basin." @default.
- W2378171806 created "2016-06-24" @default.
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- W2378171806 date "2006-01-01" @default.
- W2378171806 modified "2023-09-23" @default.
- W2378171806 title "Characteristics and origin signification of ore-forming fluid from the Jiama stratabound skarn deposit located in Gandise volcanic-magmatic arc,Tibet,China" @default.
- W2378171806 hasPublicationYear "2006" @default.
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