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RB 88/00096 Proterozoic Ediacara fauna and Cambrian archaeocyatha of the Flinders Ranges, South Australia.
This paper describes the type fossil occurrences, their present-day geological setting and, as deduced from properties of the host sediments, their interpreted palaeogeographic locations and palaeoenvironmental depositional facies which probably...-
Document
Published: 01 Jul 1988
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Beltana. Progress reports to licence expiry/renewal for the period 18/12/1967 to 17/12/1969.
An evaluation of the base metal potential of the greater Beltana 'diapiric' complex was undertaken by MIM via field mapping, soil geochemical surveys and limited shallow rotary percussion drilling at historic surface workings on small showings of...-
Document
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RB 2012/00004 MARREE, South Australia, [geological map] sheet SH54-5. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The MARREE mapsheet area includes the south-western portion of the Strzelecki Desert plus parts of the Tirari Desert, north-western Flinders Ranges and north-eastern Willouran Ranges, between latitudes 29 to 30 degrees S and longitudes 138 to 139...-
Document
Published: 01 Apr 2012
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ExpNotes MARREE: Explanatory Notes MARREE
A new generation, second edition MARREE 1:250 000 scale geological map and its explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's latest geological mapping program (1993 to...-
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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (3D pdf version 1)
Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...-
Model
- ZIP,
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Central Flinders Ranges, part PARACHILNA [mapsheet area] regional geology 3D Model (GOCAD version 1).
Upper crustal strata forming the northern to central Flinders Ranges area comprise uplifted and eroded remnants of openly folded sedimentary rocks that were deposited in an intra-continental arm of the Neoproterozoic to Early Cambrian Adelaide...-
Model
- ZIP,