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There is no abstract created for this record

An additional 12 samples were examined mainly to establish the depositional environment of the black Poltalloch clays. No marine foraminifera were found in six of the clay samples, but the microfauna of the sample taken at 63"-66" indicates deposition...

The writer accompanied by Dr. R.C. Horwitz recently traversed the Olary Broken Hill Region from Oratan Rock in South Australia to The Camel’s Humps northeast of Broken Hill, a distance of 146 miles. This reconnaissance was made between 14th and 19th...

Several general aspects of beach sand accumulation and concentration and their possible application in South Australia to known deposits and to likely source material have been considered. The coastline from Kingston in the South East to Point...

Contains a description of the biostratigraphic determinations made on drill cuttings samples recovered from below 1047 feet depth in the subject drillhole. Metamorphic basement rocks were encountered at 1191 feet depth, and drilling ceased at 1260...

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Marla 1A and 1B reached 215.30 metres and 379.40 metres respectively, penetrating aeolian sands overlying the Bulldog Shale, Cadna-owie Formation an d Observatory Hill Beds. In contrast to Byilkaoora 1, oil shows and calcite pseudomorphs after...

The fully rotary cored Oakvale 1 vertical stratigraphic drillhole was drilled by SADME Regional Geology Branch, 13 km east of Oakvale Station homestead in the north of the Murray Basin within SA, over the period 22/5/1981 to 10/6/1981. The hole was...

Forty-two thin sections collected from the Skillogalee Dolomite are representative of carbonate and non-carbonate facies, and include shales, siltstones, sandstones and conglomerates. Many of the specimens are partly or wholly stromatolitic: two...

A seismic refraction survey at Roger Corner, near Yorketown on Lower Yorke Peninsula, has profiled pre-Permian bedrock and several other shallower refractors. The survey was carried out at the request of Aberfoyle Exploration Pty Ltd, licensees of EL...

Cores taken from Barker Inlet and previous subsurface information, are used to interpret the shallow subsurface stratigraphy. Significant Holocene accumulation has taken place at Outer Harbour, Torrens Island, and the Saint Kilda intertidal flats....

Regressive intertidal sequences, with well developed zonation of flora and fauna, occur extensively around the margins of the 2 major SA gulfs and within small embayments along the exposed coastline of Eyre Peninsula. This paper summarises and...

The lowermost outcropping unit is the Bulldog Shale, overlain by the Coorikiana Sandstone, which includes a number of facies, ranging from quiet water marine to shoreline and possibly fluvial. Above is the Oodnadatta Formation. Tertiary units include...

The foraminifer, unlike any previously recorded from Etadunna Formation, is identified as Buliminoides sp. cf.B. chattonensis' (Finlay), and is compared with 3 widely separated Late Oligocene forms (New Zealand, Northern Adelaide Plains, Rhine...

The lithology and microfauna are consistent with Dry Creek Sands, of Late Pliocene age. The dominant `Marginopora vertebralis population, suggests that local Late Pliocene marine temperatures were distinctly higher than the present regime in Gulf St...

Summarises all work from 1.7.78 to 1.7.82, including bibliography of all hydrogeology and engineering geology reports for Eyre Peninsula and the Far West.

The benthonic foraminifera `Heterolepa victoriensis indicates unit is Pata Limestone of early Middle Miocene age.

Based on compilation of basement depth interpretations from previous aerial magnetic surveys.

The Kanmantoo Trough is the sedimentary and tectonic link between the Adelaide Geosyncline, and volcano - sedimentary sequences of the Tasman Fold Belt. Cambrian Flyschoid sediments were likely deposited on a marginal shelf, reflecting tectonic...