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Burial history analysis of the structurally complex eastern Officer Basin region was performed using data from petroleum, trona exploration and stratigraphic wells, seismic upholes, coal drillholes and selected seismic sections, to construct isopachs...

34 selected drill core and cuttings samples from six wells were assessed by petrographic methods for their degree of organic maturation and petroleum source potential. The sampled sequence ranged in age from ?Devonian through to Permian, Jurassic and...

TARGET:Primary target was migrating oil trapped in Algebuckina Sandstone at sites along the Cooryaninna Anticline.EXPLORATION: - Landsat survey, - reconnaissance seismic survey (Curdimurka - Marree Seismic Survey) over the Marree Block in 1985, - soil...

A description of the overall structure and stratigraphy of the Basin and identification of areas for potential coal development, based on all open file information.

Airborne and ground geophysical surveys were undertaken in the Billa Kalina area, prior to commencing to drill in a search for Olympic Dam type Cu-U-Au mineralised haematitic breccias, in order to delineate and detail several broad magnetic anomalies...

Report discusses the compilation and interpretation of 5 isopach maps prepared to illustrate spatial and temporal patterns of regional structural growth history in the Eromanga Basin sequence. The maps also provide a basis for predicting regional...

The base metal and uranium potential of a concealed Proterozoic basement high near Bulgunnia Homestead was evaluated using geological and hydrogeochemical reconnaissance and regional geophysical interpretation approaches. Seismic, ground magnetic and...

This company study of the Eromanga Basin sequence within PELs 5 and 6 and ATP 259P was designed to provide the Delhi Petroleum exploration consortium with data on the following: (a) thickness and correlation of Aptian-Albian units throughout the...

145 core samples (representing organic-rich Upper Proterozoic and Cambrian intervals in 11 wells) taken from the SADME and BMR Core Libraries were examined for palynomaceral identification and to judge levels of organic (source rock) maturity, using...

Includes Part 2 - Upper Palaeozoic and Lower Cretaceous micropalaeontology.

The Coober Pedy Opal Fields, since their discovery in 1915, have been the largest producer of precious opal in the world, with the estimated value of production over the period 1978-86 averaging $25 million per year. Mining is now done mainly by...

A summary of Block petroleum prospectivity prepared prior to starting selective low-key exploration during the 1985-1989 licence period. The report gives the rationale for the proposed work programme of 4 wells and 1900 line km of seismic acquisition...

As requested by Delhi Australian Petroleum Ltd, we have examined cuttings from Lake Frome No.1 and No.2 for microfossil remains. The wells are located in the Frome Embayment at Lat. 3 1 °03'25"S, Long. 1 39°51'52"E and Lat. 31°02'54.5"S , Long....

Four stratigraphic wells were drilled, totalling 5023 feet were drilled, Karkaro No. 1, Mount Furner No. 1, Wallira No 1 and Wallira No. 2 to verify Permian sediments and identify basement reflector. Results indicate shallow platform covered by thin...

Cootanoorina 1 was drilled about 33 miles south-southwest of Oodnadatta township by the South Australian Department of Mines, as a combined 'on structure' and stratigraphic test in the Arckaringa Sub-Basin region of the Great Artesian Basin. The main...

Mount Willoughby 1 was drilled in the northern part of the Arckaringa Basin as a continuation of the SA Department of Mines stratigraphic study of this area. The well was drilled on the western plateau of a positive gravity high on the Wintinna 1 mile...

Yardinna no. 1 well, drilled 20 miles NW of Oodnadatta township intersected the Lower Cretaceous Oodnadatta Formation and bottomed at 512 feet in Bulldog shale also of early Cretaceous age. Both the Coorikiana Sandstone Member, the basal unit of the...

Biostratigraphy of drill core and cuttings was erected for Mt Willoughby, and some biostratigraphy of the Lambina 1 was revised. Problems with contamination were encountered.

Preliminary map was prepared from mapping and shot hole logging. Precambrian crystalline basement is overlain by Permian, Mesozoic and Tertiary sediments. Younger exposed units include gypsiferous clays, sandstone and calcrete.