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GEOLOGIC CHARACTER AND GENESIS OF THE DONGZIGOU SILVER AND COPPER DEPOSIT, XINGLONG, HEBEI PROVINCE

Zhao Ying-fu

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Abstract

It is considered that the ore fluid of the deposit is origin in mantle magmatic water mixed with sea water according to the study of geologic feature, metallogenic temperature, era and matter source of the deposit. The ore matter is mainly derived from crust in depth and mantle and enriched in favourable strata and physical-chemical condition through exhalation-spout of syngenetic fault. The genesis of the deposit belongs to hydrothermal-exhalation stratabound deposit of syngenetic fault.

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What this paper is about

It is considered that the ore fluid of the deposit is origin in mantle magmatic water mixed with sea water according to the study of geologic feature, metallogenic temperature, era and matter source of the deposit. The ore matter is mainly derived from crust in depth and mantle and enriched in favourable strata and physical-chemical condition through exhalation-spout of syngenetic fault. The genesis of the deposit belongs to hydrothermal-exhalation stratabound deposit of syngenetic fault.

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Available abstract

It is considered that the ore fluid of the deposit is origin in mantle magmatic water mixed with sea water according to the study of geologic feature, metallogenic temperature, era and matter source of the deposit. The ore matter is mainly derived from crust in depth and mantle and enriched in favourable strata and physical-chemical condition through exhalation-spout of syngenetic fault. The genesis of the deposit belongs to hydrothermal-exhalation stratabound deposit of syngenetic fault.

Key concepts: Geology, Geochemistry, Hydrothermal circulation, Crust, Mantle (geology), Ore genesis, Mineralization (soil science), Metallogeny

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GEOLOGIC CHARACTER AND GENESIS OF THE DONGZIGOU SILVER AND COPPER DEPOSIT, XINGLONG, HEBEI PROVINCE — Research Paper | ScholarLens