Some high-P-subtype and low-P-subtype F-rich granites in South China

The F-rich granites in South China could be distinguished as the high-P subtype and the low-P subtype according to their P^sub 2^O^sub 5^ contents. There are obvious differences in chemical composition of these two subtypes. The high-P subtype is strongly peraluminous and characterized by low silica...

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Veröffentlicht in:	Acta geochimica 1998-10, Vol.17 (4), p.320-330
Hauptverfasser:	Chnagshi, Liu, Xiaolong, Huang, Rucheng, Wang, Lin, Yin, Xiaoming, Chen, Peirong, Chen
Format:	Artikel
Sprache:	eng
Schlagworte:	Geochemistry Granite Igneous rocks Mineralogy Phosphorus Silica Studies
Online-Zugang:	Volltext
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