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RB 2022/00010 Multi-isotopic apatite and zircon SHRIMP U–Pb geochronological results from the central-western Gawler Craton.
This report presents the results from multi-isotopic apatite and zircon SHRIMP U–Pb geochronology on thirteen samples from the central-western Gawler Craton. Eleven drill core samples are interpreted ultramafic to mafic intrusive rocks, with most...-
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Published: 01 Sep 2023
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RB 2007/00021 Compilation of SHRIMP U-Pb geochronological data for the Gawler Craton, South Australia, 2007.
This Report Book contains zircon U-Pb geochronological data obtained between December 2006 and June 2007, for rock samples derived from the Gawler Craton of South Australia. The geochronological study was undertaken as part of the National Geoscience...-
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Published: 01 Nov 2007
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RB 2012/00010 Geochronology and geochemistry of a Kimban diorite, drillhole LED001, Lake Gilles, eastern Gawler Craton.
The geology of the Lake Gilles locale in the south-west of the PORT AUGUSTA 1:250k map sheet area is poorly understood. Outcrop of basement rocks there is sparse, and typically occurs along the margins of the salt lake, where it is highly weathered....-
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Published: 01 Apr 2012
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RB 2011/00003 PACE Geochronology: Results of collaborative geochronology projects [performed during] 2009-2010.
This report book presents the results of seven geochronology research projects completed during 2009 and 2010 as a new part of the ongoing PACE Initiative geoscientific data gathering activity underwritten by the South Australian Government. It has...-
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Published: 01 Apr 2011
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RB 2013/00013 Zircon and monazite geochronology via SHRIMP and LA-ICPMS for the northern Gawler Craton, from 2009 GOMA Drilling.
The 2010 GOMA basement drilling program formed part of a collaborative ARC Linkage Project LP0882000 " Unearthing the marginal terrains of the South Australian Craton: Keystone of Proterozoic Australia " arranged between Primary Industries and...-
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Published: 01 Dec 2013
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RB 2008/00003 The Corunna Conglomerate, Gawler Craton: a review of the sedimentology and new U-Pb zircon geochronology.
The Corunna Conglomerate is a sequence of unmetamorphosed fluvial to shallow marine sediments, comprising conglomerates, sandstones and siltstones, which were deposited in active fault grabens in the eastern Gawler Craton. It is found on the...-
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Published: 01 Apr 2008