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Peachna. Progress reports, annual reports and final report to licence full surrender, for the period 22/9/1988 to 8/9/1994.
Possible economic Broken Hill - type stratiform Pb and Zn, and Middleback Range style iron ore, were targeted near Lock on central Eyre Peninsula by Western Mining Corp., who farmed-in to Stockdale's EL 1516 on March 1st, 1990 as part of a regional...-
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RB 57/00081 First report on resistivity tests in the Polda Basin.
A series of resistivity tests has been carried out in the Polda Basin in an attempt to determine whether it will be possible to map the sub surface aquifer by resistivity methods. Results indicate that this should be possible using logged boreholes...-
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Published: 01 Jan 1963
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RB 77/00074 Seismic refraction investigations in the Polda Coalfield.
A seismic cross-section along the Lock-Tuckey portion of the Polda Basin shows that bedrock is between 600 m and 900 m deep. Bedrock probably, consists of either Mt. Wedge type grits and con-glomerates or weathered crystalline basement. The basin...-
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Published: 01 Jan 1977
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RB 87/00052 Well velocity survey for drillhole CRAE KD 1A, EL 1054, Polda Basin.
The drill hole on SADME seismic line PB83-001 at shot point 338, within EL1054, aimed to provide correlation between 1983 seismic reflection profile, and the lithological and geophysical logs. Drilling to 1398 metres encountered Miocene, Eocene,...-
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Published: 01 Feb 1987
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RB 88/00006 Late Proterozoic Kilroo Formation of the Polda Basin.
Drillhole 83KD1A completed by CRA Exploration Pty Ltd In the eastern Polda Basin intersected 793 m of interlayered amygdaloidal basalts and evaporite-bearing reddish-brown mudstones below Carboniferous-Permian sediments. K-Ar geochronology and...-
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Published: 01 Jan 1988
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RB 81/00019 Tuckey no. 1 well completion report.
Tuckey 1 intersected 16 metres of Bridgewater Formation, 110.3 metres of Tertiary Poelpena Formation and 87.2 metres of Jurassic Polda Formation, which was not fully penetrated. Within the Jurassic, 4 intervals of clay and carbonaceous clay,...-
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Published: 01 Jan 1981
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RB 81/00084 Late Palaeozoic Coolardie Formation, Polda Basin.
There is no abstract created for this record-
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Published: 01 Nov 1981
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RB 85/00010 p: 21-45;Lib Geology of Eyre Peninsula.
Description of major stratigraphic and lithologic units from Archaean Sleaford Complex to Quaternary sediments, including associated granitoid suites, and their geological evolution. The geochronology and possible stratigraphic correlations of some...-
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Published: 01 Oct 1984
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RB 80/00145 Mucka Cudla no. 1 well completion report.
Based on results of SADM seismic refraction surveys Mucka Culda no. 1, 17 km NE of Colton, was drilled on shotpoint 6W of the Mount Wedge seismic traverse, for coal potential of the Polda Basin. Lignite was found in the thick Tertiary section. Absence...-
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Published: 01 Jan 1980
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RB 81/00078 Colton no. 1 well completion report.
The aim of drilling this stratigraphic hole was to evaluate the western end of the north-western lobe of the onshore Polda Basin for its stratigraphy and coal potential. Existing seismic information from this area was very poor. In terms of actual...-
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Published: 01 Sep 1981
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RB 80/00109 Biostratigraphy of Permian samples from SADME Lock no. 1, Polda Basin.
Miospores were identified in 4 of 5 samples examined.-
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Published: 01 Jan 1980
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RB 80/00108 Palynology of selected samples from Polda Basin.
5 sludge samples from boreholes mostly contain Tertiary palynomorphs and spores, with rare Jurassic palynomorphs in 1 sample. Contamination is possible and the base of the Tertiary is known to contain reworked Jurassic palynomorphs.-
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Published: 01 Jan 1980
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RB 80/00133 Palynology of selected samples from KIMBA 1:250 000 sheet Eyre Peninsula no. 2.
2 of 3 samples are suggested to be Cainozoic.-
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Published: 01 Jan 1980
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RB 81/00109 Lock no. 1 well completion report.
The aim was to core Palaeozoic units occurring between Late Jurassic (Polda Formation) and Precambrian basement rocks. The hole was abandoned at 369 metres well before the prognosed basement depth of 650 metres. Intersected were : 2 metres of...-
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Published: 01 Jan 1982
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RB 81/00116 Late Jurassic Polda Formation, Eyre Peninsula.
There is no abstract created for this record-
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Published: 01 Jan 1982
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RB 90/00074 Explanatory Notes for the ELLISTON 1:250 000 map sheet.
There is no abstract created for this record-
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Published: 01 Nov 1990
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RB 96/00010 Musgrave Proclaimed Wells Area groundwater assessment.
The County Musgrave Proclaimed Wells Area on Eyre Peninsula, situated mainly near Elliston and extending eastwards towards Lock, contains a number of small groundwater lenses of potable quality which are surrounded by brackish to saline groundwater....-
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Published: 01 Jan 1994
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RB 97/00027 Further palynological dating and correlation of Mesozoic and Tertiary sediments from Eyre Peninsula, SA.
Two groups of samples from Eyre Peninsula have been analysed. The Elliston samples are correlative with the Polda Formation, probably in the latest Middle Jurassic. The younger Middle Eocene E04-1 sample indicates the presence of Pidinga Formation,...-
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Published: 01 Jul 1997
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RB 93/00002 Palynological dating of borehole samples from the Polda Basin area, Eyre Peninsula.
There is no abstract created for this record-
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Published: 01 Jan 1993
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RB 92/00009 Preliminary palynological dating of borehole samples from the Polda Basin, Eyre Peninsula.
19 samples of exploratory RC aircore drillhole cuttings were examined by a SADME consultant to determine their microfloral assemblages, and to date the host sediments by correlation of diagnostic palynomorphs with published biostratigraphic schemes.-
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