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- W2381042954 abstract "From Xiaguan to Erlangping in Henan gold deposits (mineralized pits) occur extensively; they vary in mineralization type and their conditions of occurrence are complex. Gold deposits formed in intrusive bodies and contact zone between intrusive bodies and wall rocks, and in Mesoproterozoic and early Palaeozoic strata. The authors divide gold deposits in contact zones and strata into five types on the basis of ore source, metallogenic fluid origin and mineralization mechanism. The gold deposits are formed because of magma hydrothermalism, metamorphic hydrothermalism and hydrothermal superimposion on the background of volcanism, volcanic sedimentation and normal sedimentation. Each type of gold deposits is experienced multiphase and polystage mineralization, but mainly late hydrothermal replacement and packing mineralization. Tectonics controls the formation of gold deposits distinctly. The regional deep fault belt controls gold deposits belt. Second-order ductile-brittle shear belt controls the distribution of gold deposits; three-order tectonics of interlayer fractured zones, fracture crack zones and contact zones control the ore forming. In all, the main mineralization was hydrothermal superimposion or regeneration." @default.
- W2381042954 created "2016-06-24" @default.
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- W2381042954 date "2005-01-01" @default.
- W2381042954 modified "2023-09-28" @default.
- W2381042954 title "Geological features and metallogenic model of hydrothermal superimposion (regeneration) gold deposits from Xiaguan to Erlangping in Henan" @default.
- W2381042954 hasPublicationYear "2005" @default.
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