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https://doi.org/10.1007/bf0318...
Article . 1982 . Peer-reviewed
License: Springer TDM
Data sources: Crossref
https://dx.doi.org/10.1007/bf0...
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The evolution of alkali elements and the division of geochemical process for pegmatite Vein No. 3, Altai, Xinjiang, China

descriptionPublicationkeyboard_double_arrow_right Article , Other literature type 01 Oct 1982 English Publisher:Springer Science and Business Media LLCJournal:Geochemistry, volume 1, pages 435-441 (issn: 0253-486X, Copyright policy )
Authors: Xianjue Wang;

doi: 10.1007/bf03180348

The evolution of alkali elements and the division of geochemical process for pegmatite Vein No. 3, Altai, Xinjiang, China

Abstract

According to the evolution of alkali elements (e.g. K, Na, Li) and the relationship among them in the melt-solution of pegmatitic magma, the author divides the pegmatitic process for Vein No. 3 into three main geochemical stages associated with mineralization, i.e., K-Na, Na-Li and K stages. The above division scheme has been proved to be valid by field geological survey and laboratory data from thermodynamic analyses.

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selected citations
These citations are derived from selected sources.
This is an alternative to the "Influence" indicator, which also reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Citations provided by BIP!
popularity
This indicator reflects the "current" impact/attention (the "hype") of an article in the research community at large, based on the underlying citation network.
BIP!Popularity provided by BIP!
influence
This indicator reflects the overall/total impact of an article in the research community at large, based on the underlying citation network (diachronically).
BIP!Influence provided by BIP!
impulse
This indicator reflects the initial momentum of an article directly after its publication, based on the underlying citation network.
BIP!Impulse provided by BIP!
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