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GEOLOGICAL CHARACTERISTICS AND GENESIS OF DEPOSIT IN GUANLINGGENG Pb-Zn MINE

Libo Wang

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Abstract

Guanlinggeng Pb-Zn mine is located at Caledonian tectonic zone in Guanzi Township and Taiyangsi area of northern belt of west Qinling. In order to reveal the metallogenetic regularity of multi-metal and ore-control factors in this area, metallogenetic conditions have been studied from such factors as the regional geological setting and geochemistry, ore-beating formation and metallogenetic structures, it is supposed that Guanlinggeng Pb-Zn deposit is a magamatic hydrothermal deposit of medium-low temperature, obviously controlled by the fault, the data of trace elements and S-isotope show that the sources of ore-forming material is in deep, the metallogenetic stages should be previously divided into 3 periods.

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What this paper is about

Guanlinggeng Pb-Zn mine is located at Caledonian tectonic zone in Guanzi Township and Taiyangsi area of northern belt of west Qinling. In order to reveal the metallogenetic regularity of multi-metal and ore-control factors in this area, metallogenetic conditions have been studied from such factors as the regional geological setting and geochemistry, ore-beating formation and metallogenetic structures, it is supposed that Guanlinggeng Pb-Zn deposit is a magamatic hydrothermal deposit of medium-low temperature, obviously controlled by the fault, the data of trace elements and S-isotope show that the sources of ore-forming material is in deep, the metallogenetic stages should be previously divided into 3 periods.

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Available abstract

Guanlinggeng Pb-Zn mine is located at Caledonian tectonic zone in Guanzi Township and Taiyangsi area of northern belt of west Qinling. In order to reveal the metallogenetic regularity of multi-metal and ore-control factors in this area, metallogenetic conditions have been studied from such factors as the regional geological setting and geochemistry, ore-beating formation and metallogenetic structures, it is supposed that Guanlinggeng Pb-Zn deposit is a magamatic hydrothermal deposit of medium-low temperature, obviously controlled by the fault, the data of trace elements and S-isotope show that the sources of ore-forming material is in deep, the metallogenetic stages should be previously divided into 3 periods.

Key concepts: Geology, Hydrothermal circulation, Geochemistry, Tectonics, Fault (geology), Mining engineering, Paleontology

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GEOLOGICAL CHARACTERISTICS AND GENESIS OF DEPOSIT IN GUANLINGGENG Pb-Zn MINE — Research Paper | ScholarLens