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- W2384751808 abstract "The hypo-volcanic crytoexplosion Breccia rock body(vein) is formed of granite magma,which is rise to the lower of the earth's crust along the east-western shear zone and exploded below the Archean fundus rock.The felstone vein and the hypo-volcanic crytoexplosion Breccia rock are from the same magma source,and are formed in the different evolution stages.Both of them the affinity with the gold mineralization,the geochemistry characteristic of the lanthanon,microelement and isotope shows that the main mineralization material and liquid have the same source with them.The hypo-volcanic crytoexplosion Breccia rock body(vein) and the felstone in the east-western shear zone are the important symbol of the exploration." @default.
- W2384751808 created "2016-06-24" @default.
- W2384751808 creator A5023311855 @default.
- W2384751808 date "2008-01-01" @default.
- W2384751808 modified "2023-09-23" @default.
- W2384751808 title "The Geology Characteristic of the Hypo-Volcanic Crytoexplosion Rytoexplosion Breccias of the Xiangluwanzi Gold Zone And the Relation With the Gold Deposit" @default.
- W2384751808 hasPublicationYear "2008" @default.
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