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- W2356583593 abstract "Several intrusive rock relative hydrothermal solution type gold deposits compose the Laozhashan gold ore field. The ore bodies are mainly veins and occurred in the skarn of Paleo-Proterozoic Xingdong Group Damahe Formation. The type of the ores are mainly skarn disseminated gold ore, secondly are breccia disseminated. The mineralization could be parted into two stages: the early stage is migmatized hydrothermal solution of Proterozoic that rich As and short S in high temperature come into being migmatized hydrothermal solution type gold body. The late stage one is the regenerated magma hydrothermal of Yanshan period superimposed on the early ore body and enriched the early one. NE strike fault controlled the gold deposit and NW and NWW strike faults and ductile shear zone controlled the gold ore body. The genesis of the gold deposit is late hydrothermal superimposed migmatization replace skarn type gold deposit." @default.
- W2356583593 created "2016-06-24" @default.
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- W2356583593 date "2004-01-01" @default.
- W2356583593 modified "2023-09-25" @default.
- W2356583593 title "The genesis of the southeast section of the Laozhashan gold ore field, Heilongjiang" @default.
- W2356583593 hasPublicationYear "2004" @default.
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