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- W2357536741 abstract "Gold deposits at Shangmanggang can be divided into laterite-type and Carlin type. These two kinds of gold deposits, which overlap each other in space, are controlled by the Shangmanggang fault. As, Hg, Au, Sb and Mo elements have same characteristics in red-clay profile, which is similar to Carlin type gold deposit. These deposits are rich in Cs and U, relatively lack of Ba and Sr. Chondrite standardized modes of REE show that LREE is richer than HREE in both laterite-type and Carlin-type gold deposit. Carlin type gold deposit was formed in the Cretaceous period and laterite-type gold deposit formed in the Pliocene. Mineralizing times of these two type deposits has precedence." @default.
- W2357536741 created "2016-06-24" @default.
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- W2357536741 date "2003-01-01" @default.
- W2357536741 modified "2023-09-27" @default.
- W2357536741 title "RELATIONS OF CARLIN-TYPE AND LATERITE-TYPE GOLD DEPOSITS AT SHANGMANGGANG, WESTERN YUNNAN PROVINCE" @default.
- W2357536741 hasPublicationYear "2003" @default.
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