-
RB 93/00010 Explanatory Notes for the WARRINA 1:250 000 geological map.
The oldest rocks on WARRINA outcrop in the Peake and Denison Inliers, which comprise the Davenport and Denison Ranges and small inliers to the east. Basement in this area consists of Palaeoproterozoic metamorphic rocks which were intruded by...-
Document
Published: 01 Jun 1994
-
RB 96/00019 Correlation of Permian sandstones in the Officer, Arckaringa and Pedirka Basins.
A detailed petrographic study of Permian sandstone drill cuttings and core samples selected from 32 drillholes variously located within the Officer, Arckaringa and Pedirka Basins was undertaken, with the intent of trying to classify the sandstones as...-
Document
Published: 01 Oct 1997
-
Nilpinna Homestead area (part of the Australian Diamond Exploration joint venture). Progress reports and final report to licence expiry/full surrender, for the period 16/1/1980 to 22/2/1987.
Diamond exploration undertaken in the Peake and Denison Ranges included the acquisition and processing of aerial magnetic, radiometric and heliborne magnetic and VLF-EM surveys, with follow-up ground magnetic and Sirotem surveys, plus extensive...-
Document
-
1982 seismic survey, Christmas Creek, final report.
AIM:The 1982 Christmas Creek Seismic Survey was designed to cover a wide area of the sparsely explored western farmout blocks of PELs 5 and 6, where Eromanga Basin sediments thin and overly sub-basins of variously aged prospective sediments. Primary...-
Document
-
Pedirka Sector: a reassessment of geology, porosity, maturity and maturity history.
A review of the Permo-Triassic and Mesozoic distribution of reservoir units. Data for some Birdsville Track Ridge wells are included as the development of the Pedirka Sector basins and the Birdsville Track Ridge are closely related.-
Document
-
Organic petrology of samples from a selected group of wells in or near the Arckaringa Block.
Nineteen drill cuttings and 15 drill core samples of Permian, Cretaceous and Jurassic ages were assessed for organic maturation and source rock potential.-
Document
