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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2006-03
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Characteristics and origin signification of ore-forming fluid from the Jiama stratabound skarn deposit located in Gandise volcanic-magmatic arc,Tibet,China

YAO Peng~(1,2),GU Xue-xiang~(1,3), LI Jin-gao~4,FAN Wen-yu~21.College of Earth Sciences,Chengdu University of Technology,Chengdu 610059,China;2.Chengdu Institute of Geology and Mineral Resources,Chengdu 610082,China;3.Institute of Gechemistry,Chinese Academy of Sciences,Guiyang 550002,China;4.Xizang Bureau of Geology and Mineral Resources,Lhasa 850000,China  
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.
【Fund】: 科技部重点基础前期研究专项(2003CCA019);; 南京大学成矿作用国家重点试验室开放研究基金;; 原地矿部定向基金(地科97-20)联合资助项目
【CateGory Index】: P618.41
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