-
RB 2007/00002 Commonwealth Hill magnetic anomaly, north-western Gawler Craton: an interpretation and results of zircon LA-ICPMS U-Pb dating.
High precision geochronological analyses of metamorphic and inherited magmatic zircon grains, which were obtained from stored percussion drillhole samples of a garnet gneiss that occurs within the Commonwealth Hill magnetic anomaly, north-western...-
Document
Published: 01 Jan 2007
-
RB 2013/00021 Reconnaissance LA-ICPMS zircon U-Pb geochronology from samples from the central-northern Gawler Craton.
The laser ablation - inductively coupled plasma mass spectrometry (LA-ICPMS) U-Pb zircon geochronology data reported herein derive from three rock samples sourced from the central - northern Gawler Craton, South Australia. These samples have been...-
Document
Published: 01 Jan 2013
-
RB 2009/00016 Compilation of Shrimp U-Pb geochronological data for the Mulgathing Complex, Gawler Craton, South Australia, 2007-2009.
This report book contains SHRIMP zircon U-Pb geochronological data obtained between July 2007 and June 2009, for 10 metasedimentary and meta-igneous rocks from the Mulgathing Complex of the north-estern Gawler Craton. The geochronological study was...-
Document
Published: 01 Aug 2009
-
RB 2022/00008 Zircon LA–ICP–MS geochronological and geochemical results from the central-western Gawler Craton.
This report presents the results from zircon LA–ICP–MS U–Pb geochronological age determinations, and both trace and rare earth element abundance geochemical analyses, performed on fifteen outcrop and drill core samples originating from the...-
Document
Published: 01 Nov 2022
-
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...-
Document
Published: 01 Sep 2023
