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- W2372124227 abstract "Highly evolved phosphorous-rich peraluminous magmatic system shows distinctive geochemical behaviors.It was characterized as being high in P,and ASI,low in Ca,Mg and Fe,strong depletions in REE,Th and Y, and mineralizations of W,Sn,Nb and Ta.The alkali feldspar crystallized from the P-rich peraluminous magmatic system is often enriched in phosphorous.The abundance and distribution of phosphorus in alkali feldspar can reveal the evolution history of the magma.As P has strong affinity to Li,an assemblage of spodumene-amblygonite-montebrasite occurred in the last stage of magmatic evolution.Previous studies showed that phosphorus can depress the liquidus and solidus,decrease the viscosity and increase the solubility of water in haplogranite melts.However,there remain some issues in the P-rich magmatic system to be explored clearly in the future,such as the effects of phosphorus on liquid immiscibility,fractionation of REE and other incompatible elements,and mineralizations of the rare metals." @default.
- W2372124227 created "2016-06-24" @default.
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- W2372124227 date "2008-01-01" @default.
- W2372124227 modified "2023-09-23" @default.
- W2372124227 title "THE CURRENT STATUS AND PROBLEMS IN THE STUDIES OF THE PHOSPHOROUS-RICH PERALUMINOUS MAGMATIC SYSTEM" @default.
- W2372124227 hasPublicationYear "2008" @default.
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