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《Earth Science Frontiers》 2001-04
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GENETIC RELATION BETWEEN DEEP-SEATED ALKALI- RICH HYDROTHERMAL FLUIDS AND ORE-BEARING PORPHYRIES OF PORPHYRY COPPER DEPOSITS EVIDENCE FROM FLUID INCLUSIONS AND PHENOCRYST TEXTURES

CHEN Wen ming (Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)  
Detailed study of the textures and fluid inclusions of phenocrysts in ore bearing porphyries of several major porphyry copper deposits in China indicates that the phenocrysts in porphyroblastic textures are of distinct poikilitic, sieve, interstitial, glomeoprphyritic and overgrowth textures. The fluid inclusions in the phenocrysts (quartz) show the features of the assemblage of saturated and oversaturated saline water vapor boiling fluid inclusions and are lacking in melt inclusions. In this boiling fluid inclusion assemblage (whole rock), the oversaturated saline water inclusions make up 29%, saturated saline water inclusion 2%, unsaturated inclusions 45% and vapor inclusions 24% of the assemblage. The formation temperatures of the phenocrysts estimated by homogenization temperatures of saturated saline water inclusion range from 311 ℃to 407℃. The fluid inclusions are dominantly composed of H 2O, CO 2, K +, Na +, Cl -, and SO 2- 4, thus further validating that the ore bearing porphyries in porphyry copper deposits are not the product of direct magmatic crystallization but most likely to be the result of metasomatism or partial melting of the upper copper bearing silicate crust by deep seated K and Na rich siliceous hydrothermal fluids.
【Fund】: 国家自然科学基金资助项目 ( 49970 32 )
【CateGory Index】: P588.12
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