Tectono-thermal evolution of the Palaeoproterozoic Granites–Tanami Orogen, North Australian Craton: Implications from hornblende and biotite 40Ar/39Ar geochronology

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Tectono-thermal evolution of the Palaeoproterozoic Granites–Tanami Orogen, North Australian Craton: Implications from hornblende and biotite 40Ar/39Ar geochronology

The Palaeoproterozoic Granites–Tanami Orogen (GTO) hosts a number of gold deposits located in the southern margin of the North Australian Craton. The major stratigraphic succession is the Palaeoproterozoic Tanami Group which is subdivided into the Dead Bullock Formation and conformably overlying Kil...

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Bibliographic Details
Main Authors:	Li, B., Bagas, L., Jourdan, Fred
Format:	Journal Article
Published:	Elsevier BV 2014
Subjects:	Cooling age Tanami Group Back-arc basin basalt 40Ar/39Ar geochronology Tectono-thermal event Recrystallization age
Online Access:	http://hdl.handle.net/20.500.11937/32689

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