2011Mineral ExplorationRequires access

The matallogenic system and the prognosis,Dabaoshan Mo-Cu-Pb-Zn deposit,Guangdong province

Gao Zhi-hui

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Abstract

The Dabaoshan polymetallic deposit containing aboundant copper,lesd and zinc mineral resouces.A significant process is that porphyry W-Mo mineralizaton system was discovered,with huge-scale prospective on top of the granite-porphyry,Iron deposit is weathering and leaching type one.Nonferrous metals mineralization is associated with magmatic hydrothermal process.It is established that the Daobaoshan porphyry metallogenic system,which granite porphyry is the ore-forming intrusion,Mo-W deposit occurred in the ore-forming center,with skarn-type Mo,vein-type Cu,Cu-Pb-Zn,Pb-Zn,Pb-Zn-Ag,and siderite veins gradually far away from this center.It is studied that the ore-forming depth and erosion level.The depth of the porphyry-type metallogenic system is more than 2000 meters,and that of erosion is more than 1500 meters(not includes that destroyed by fault).The important prospecting target shonld include three aspects: 1) Beyond the eastern boundary of the porphyry Mo mineralization system;2) the other side of the porphyry Mo deposit under the fault;3) NNW area of the porphyry,and porphyry type and skarn type Mo-W deposits around Chuandu intrusion.

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The Dabaoshan polymetallic deposit containing aboundant copper,lesd and zinc mineral resouces.A significant process is that porphyry W-Mo mineralizaton system was discovered,with huge-scale prospective on top of the granite-porphyry,Iron deposit is weathering and leaching type one.Nonferrous metals mineralization is associated with magmatic hydrothermal process.It is established that the Daobaoshan porphyry metallogenic system,which granite porphyry is the ore-forming intrusion,Mo-W deposit occurred in the ore-forming center,with skarn-type Mo,vein-type Cu,Cu-Pb-Zn,Pb-Zn,Pb-Zn-Ag,and siderite veins gradually far away from this center.It is studied that the ore-forming depth and erosion level.The depth of the porphyry-type metallogenic system is more than 2000 meters,and that of erosion is more than 1500 meters(not includes that destroyed by fault).The important prospecting target shonld include three aspects: 1) Beyond the eastern boundary of the porphyry Mo mineralization system;2) the other side of the porphyry Mo deposit under the fault;3) NNW area of the porphyry,and porphyry type and skarn type Mo-W deposits around Chuandu intrusion.

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Available abstract

The Dabaoshan polymetallic deposit containing aboundant copper,lesd and zinc mineral resouces.A significant process is that porphyry W-Mo mineralizaton system was discovered,with huge-scale prospective on top of the granite-porphyry,Iron deposit is weathering and leaching type one.Nonferrous metals mineralization is associated with magmatic hydrothermal process.It is established that the Daobaoshan porphyry metallogenic system,which granite porphyry is the ore-forming intrusion,Mo-W deposit occurred in the ore-forming center,with skarn-type Mo,vein-type Cu,Cu-Pb-Zn,Pb-Zn,Pb-Zn-Ag,and siderite veins gradually far away from this center.It is studied that the ore-forming depth and erosion level.The depth of the porphyry-type metallogenic system is more than 2000 meters,and that of erosion is more than 1500 meters(not includes that destroyed by fault).The important prospecting target shonld include three aspects: 1) Beyond the eastern boundary of the porphyry Mo mineralization system;2) the other side of the porphyry Mo deposit under the fault;3) NNW area of the porphyry,and porphyry type and skarn type Mo-W deposits around Chuandu intrusion.

Key concepts: Skarn, Geology, Mineralization (soil science), Geochemistry, Prospecting, Porphyry copper deposit, Hydrothermal circulation, Fluid inclusions

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The matallogenic system and the prognosis,Dabaoshan Mo-Cu-Pb-Zn deposit,Guangdong province — Research Paper | ScholarLens