Geological Features and Prospecting Signs of Mo-Polymetallic Ore Field in Hekanzi
Zhao Shu-tang
Abstract
Zhao Shu-tang
Abstract
Hekanzi Mo-polymetallic deposit is located in northeast part of Lingyuan-Xifengkou gold ore zone.At space-time and genesis,it proved that mineralization was distinctly contact with the later Yanshan period complex-rock mass,that introuded in the northeast's Hekanzi-Syncline.Formed contact zones'Au-Cu-mineralization between Biotite-granite and Dolomitic-limestone of Wumishan-Formation,Biotite-granite's gold mineralization,and Porphyry type Mo-mineralization in K-granite.By analyzing geological characters of the deposit,the further genetic laws of the ore is sumed up,and it is considered preliminary that,there is a good prospect in ore-finding.
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Hekanzi Mo-polymetallic deposit is located in northeast part of Lingyuan-Xifengkou gold ore zone.At space-time and genesis,it proved that mineralization was distinctly contact with the later Yanshan period complex-rock mass,that introuded in the northeast's Hekanzi-Syncline.Formed contact zones'Au-Cu-mineralization between Biotite-granite and Dolomitic-limestone of Wumishan-Formation,Biotite-granite's gold mineralization,and Porphyry type Mo-mineralization in K-granite.By analyzing geological characters of the deposit,the further genetic laws of the ore is sumed up,and it is considered preliminary that,there is a good prospect in ore-finding.
Key concepts: Mineralization (soil science), Prospecting, Geology, Biotite, Geochemistry, Syncline, Contact zone, Geomorphology