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- W2391745444 abstract "Laerma and Xiajiadian gold depeosits are all located in the sedimentary domain of palaeozoic taphrogeosyncline and hosted in carbonaceous-siliceous-limy sediments and characterized by micro-disseminated Au. The two deposits occur at different localities and they are similar and different in geological background, ore-controlling factors, geological and geochemical characteristics, ore-forming epoch, ore type and genesis etc. H-isotope values indicate that ore fluid in Xiajiadian gold deposit is characteristic of metamorphic water. Their Pb-isotope values fall between the boundaries of upper crustal and orogenic fields showing that they are dynamically formed by orogeny. Their REE patterns decline slightly to right and imply inheritable relation between the deposits and their wall rocks. They are of Carlin-like gold deposits." @default.
- W2391745444 created "2016-06-24" @default.
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- W2391745444 date "2004-01-01" @default.
- W2391745444 modified "2023-09-25" @default.
- W2391745444 title "THE CHARACTERISTIC CONTRAST OF GEOLOGY AND GEOCHEMISTRY IN LAERMA GOLD DEPOSIT AND XIAJIADIAN GOLD DEPOSIT" @default.
- W2391745444 hasPublicationYear "2004" @default.
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