Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block

Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern... •The Nage peraluminous granitoids in the Yangtze Block were formed at ca. 850 Ma.•The granitic magma had high temperature but low oxygen fugacity.•Fractional crystallization played a role in determining the geochemical composition.•Extension along the southern margin of the Yangtze Block occurred at ca. 850 Ma. http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Precambrian Research Elsevier

Identification of ca. 850 Ma high-temperature strongly peraluminous granitoids in southeastern Guizhou Province, South China: A result of early extension along the southern margin of the Yangtze Block

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Publisher
Elsevier
Copyright
Copyright © 2018 Elsevier B.V.
ISSN
0301-9268
eISSN
1872-7433
D.O.I.
10.1016/j.precamres.2018.02.007
Publisher site
See Article on Publisher Site

Abstract

•The Nage peraluminous granitoids in the Yangtze Block were formed at ca. 850 Ma.•The granitic magma had high temperature but low oxygen fugacity.•Fractional crystallization played a role in determining the geochemical composition.•Extension along the southern margin of the Yangtze Block occurred at ca. 850 Ma.

Journal

Precambrian ResearchElsevier

Published: May 1, 2018

References

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