-
Mount Willoughby, Marla, Nicholson Hill, Hope, Manya, Emu, Moorefield, Lake Meramangye, Dingo Claypan and Alinya (Officer Basin). Progress, technical and partial relinquishment reports for the period 20/8/1980 to 19/8/1985.
TRONA EXPLORATION: Of the 9 rotary/diamond holes drilled, only the first, Meramangye 1, intersected a unit equivalent to the Observatory Hill Beds, which was the target horizon for trona. Drillholes Manya nos 2-6 and Marla 7 intersected Cambrian red...-
Document
-
1974 seismic survey, Everard, final report.
AIM:The 1974 Everard Seismic Survey consisted of a detailed grid of 103 km over the Munyarai prospect, and a regional tie line of 54 km with outcrops at the rim of the Officer Basin, to investigate the possibility of a prospective Ordovician sequence...-
Document
-
1993 Wallatinna seismic survey, final report.
AIM: The MESA Wallatinna Seismic Survey was programmed to provide sufficient new data on the eastern Officer Basin, together with petrophysics and petroleum geochemical updates, to stimulate renewed interest and reduce exploration risk such that in...-
Document
-
Summary of seismic interpretation, Marla area, Officer Basin.
Modern, multifold seismic data over the far eastern Officer Basin have been reinterpreted and seven reflectors mapped in time. Parts of six major structural zones are identified in the region: Munyarai Tough, Marla Overthrust Zone, Ammaroodinna...-
Document
Published: 31 Jan 1993
-
RB 72/00121 Explanatory Notes for the EVERARD 1:250 000 geological map.
Pronounced positive and negative geophysical anomalies on EVERARD represent the crystalline Musgrave Block in the north, a basement trough more than 4 km in depth that flanks the Musgrave Block to the south, and the crystalline Ammaroodinna Inlier to...-
Document
Published: 03 Jul 1972
-
RB 73/00181 Seismic investigations of the Wintinna Trough, 1972.
Seismic refraction and reflection work in the Wallatinna area in 1972 has suggested a fault along the north west edge of the Ammaroodinna inlier as the north west limit of Permian sedimentation, and thus of the Arckaringa basin. This is probably not...-
Document
Published: 08 Aug 1973
-
RB 2014/00005 WINTINNA, South Australia, [geological map] sheet SG53-14. South Australia. Geological Survey. 1:250 000 Series - Explanatory Notes.
The WINTINNA 1:250 000 mapsheet area lies between latitudes 27° to 28° South and longitudes 133°30’ to 135°00’ East. This ~16 400 square km area includes the Marla and Cadney Park settlements, and is crossed by the Stuart Highway and Adelaide to...-
Document
Published: 01 Mar 2015
-
Northern Gawler Province regional geology 3D Model (GOCAD version 1).
Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...-
Model
- ZIP,
-
Northern Gawler Province regional geology 3D Model (3D pdf version 1)
Large potential field anomalies can be observed in the Marla region of northern South Australia, and have been used to define the northern limit of the Gawler Craton. The subject project’s aim was to model the plausible source(s) for each of those...-
Model
- ZIP,
-
ExpNotes EVERARD: Explanatory Notes EVERARD, SG 53-13.
There is no abstract created for this record.-
Document
-
ExpNotes WINTINNA: Explanatory Notes WINTINNA, SG 53-14.
A new generation, first edition WINTINNA 1:250 000 scale geological map and explanatory notes have been published. These documents represent the conclusion of the Geological Survey of South Australia's geological mapping program undertaken in the...-
Document
