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GSWA Explanatory Notes
Department of Mines, Petroleum and Exploration
Geological Survey of
Western Australia
www.dmpe.wa.gov.au
 
Amadeus Basin (Phase 1) (NA)
PW Haines, HJ ALLEN, and RM Hocking
 
Type
Basin
Lithology
sedimentary rocks
Parent unit
Centralian Superbasin
Child units
Child Units
Constituent lithostratigraphic units
––
Affected by events
Delamerian Orogeny
Petermann Orogeny
Tectonic setting
basin: intracratonic basin
 
Summary
No summary narrative found.
 
Distribution
No distribution narrative found.
 
Description
No description narrative found.
 
Geochronology
  
Amadeus Basin (Phase 1)
Maximum age
Minimum age
Age (Ma)
1000
510
Age
Neoproterozoic
Paleozoic
No geochronology narrative found.
 
Contact relationships
   
No contact relationship narrative found.
 
Tectonic setting
No tectonic setting narrative found.
BookMark
Child units
   
Tectonic unit name
Unit code
Age (Ma)
Type
Amadeus Basin (Phase 1), Baron Inlier
NAB
850–510
Inlier/Outlier
 
Recommended reference for this publication
Haines, PW, ALLEN, HJ and Hocking, RM (partial report), Amadeus Basin (Phase 1) (NA): Geological Survey of Western Australia, WA Geology Online, Explanatory Notes extract, viewed 17 January 2026. <www.dmpe.wa.gov.au/ens>
 
This page was last modified on 16 February 2024.
 
 
Grid references in this publication refer to the Geocentric Datum of Australia 1994 (GDA94) or 2020 (GDA2020). Locations mentioned in the text are referenced using Map Grid Australia (MGA) coordinates, Zones 49 to 52. No conversion from GDA94 to GDA2020 has been applied to coordinates quoted for units published prior to October 2025. All locations are quoted to at least the nearest 100 m.
 
Capitalized names in text refer to standard 1:100 000 map sheets, unless otherwise indicated.
 
WAROX is GSWA’s field observation and sample database. WAROX site IDs have the format ‘ABCXXXnnnnnnSS’, where ABC = geologist username, XXX = project or map code, nnnnnn = 6 digit site number, and SS = optional alphabetic suffix (maximum 2 characters).
 
Unless otherwise stated, all isotopic ages are based on U–Pb analysis of zircon and quoted within 95% uncertainties, with U–Pb measurements collected using a sensitive high-resolution ion microprobe (SHRIMP) in the John de Laeter Centre at Curtin University, Perth, Western Australia.
 
Digital data related to WA Geology Online, including geochronology and digital geology, are available online at the Department’s Data and Software Centre and may be viewed in map context at GeoVIEW.WA.
 
Further details of geological publications and maps produced by the Geological Survey of Western Australia are available from <www.dmpe.wa.gov.au/GSWApublications>.