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

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

Internet

http://hdl.handle.net/20.500.11937/32689

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