Zircon U–Pb ages of the pegmatites in the Kontum massif, central Vietnam and their quality evaluation for ceramic industry

Pegmatites occur in the Kontum massif as NE–SW oriented large dykes ranging from a few meters to several tens of meters in width. They consist of 3 stages of formation based on the difference of petrographic characteristics and ages: the first–stage pegmatites are characterized by quartz (40–45 vol%...

Ausführliche Beschreibung

Gespeichert in:

Bibliographische Detailangaben
Veröffentlicht in:	Journal of Mineralogical and Petrological Sciences 2021, Vol.116(6), pp.279-292
Hauptverfasser:	CUONG, Truong Chi, HIEU, Pham Trung, MINH, Pham, KAWAGUCHI, Kenta, ANH, Nong Thi Quynh, HUNG, Khuong The
Format:	Artikel
Sprache:	eng
Schlagworte:	Biotite Ceramic Ceramics Ceramics industry Chronology Colour Feldspars Grain size Granite Kontum massif Lead isotopes Magma Massifs Mica Muscovite Ocean basins Ordovician Pegmatite Permian Quality assessment Quartz Radiometric dating Silurian Triassic Zircon Zircon U–Pb dating
Online-Zugang:	Volltext
Tags:	Tag hinzufügen Keine Tags, Fügen Sie den ersten Tag hinzu!

Beschreibung
Zusammenfassung:	Pegmatites occur in the Kontum massif as NE–SW oriented large dykes ranging from a few meters to several tens of meters in width. They consist of 3 stages of formation based on the difference of petrographic characteristics and ages: the first–stage pegmatites are characterized by quartz (40–45 vol%) and K–feldspar (55–60 vol%), the second–stage pegmatites are composed of K–feldspar (70 vol%), quartz (25 vol%), muscovite (
ISSN:	1345-6296 1349-3825
DOI:	10.2465/jmps.210911