Data

L038 Quilpie-Eromanga seismic reflection survey, QLD, 1959

Geoscience Australia
Bigg-Wither, A.L. ; Morton, A.G.
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=https://pid.geoscience.gov.au/dataset/ga/76397&rft.title=L038 Quilpie-Eromanga seismic reflection survey, QLD, 1959&rft.identifier=https://pid.geoscience.gov.au/dataset/ga/76397&rft.publisher=Geoscience Australia&rft.description=A reconnaissance seismic survey was made in the area of Quilpie and Et.omanga in south-western Queensland. Traverses crossed the Harkaway, Pinkilla, and Tallyabra Domes. Reflection horizons were correlated with horizons within the Mesozoic sediments, and one persistent reflection was correlated with a horizon near the top of the Palaeozoic sediments. A thickness of sediments of up to 15,000 ft, including up to 11,000 ft of Palaeozoic rocks, was indicated on the flanks of the Harkaway and Pinkilla Domes. Results were compared with existing gravity data. Suggestions of faulting are based on seismic and gravity evidence taken together and also on gravity evidence alone in locations not covered by the seismic work.Maintenance and Update Frequency: asNeededStatement: Geological reconnaissance work by Geosurveys Ltd, on behalf of L.H. Smart Oil Exploration Pty Ltd, has disclosed the presence of numerous well-exposed anticlines in the Quilpie/Eromanga area of south-west Queensland, most of which appear to have been unrecognised previously. A broad reconnaissance gravity survey was also made and there was generally good correlation between these surface structures and the observed Bouguer anomalies, suggesting that the structures continued at depth.^To investigate the area further, the Bureau of Mineral Resources carried out a seismic survey.&rft.creator=Bigg-Wither, A.L. &rft.creator=Morton, A.G. &rft.date=1962&rft.coverage=westlimit=142.0; southlimit=-27.0; eastlimit=145.0; northlimit=-26.0&rft.coverage=westlimit=142.0; southlimit=-27.0; eastlimit=145.0; northlimit=-26.0&rft_rights=&rft_rights=Creative Commons Attribution 4.0 International Licence&rft_rights=CC-BY&rft_rights=4.0&rft_rights=http://creativecommons.org/licenses/&rft_rights=WWW:LINK-1.0-http--link&rft_rights=Australian Government Security ClassificationSystem&rft_rights=https://www.protectivesecurity.gov.au/Pages/default.aspx&rft_rights=WWW:LINK-1.0-http--link&rft_rights=Creative Commons Attribution 4.0 International Licence http://creativecommons.org/licenses/by/4.0&rft_subject=geoscientificInformation&rft_subject=Seismology and Seismic Exploration&rft_subject=EARTH SCIENCES&rft_subject=GEOPHYSICS&rft_subject=HVC_144637&rft_subject=Seismic Data seismic survey&rft_subject=seismic reflection&rft_subject=seismic refraction&rft_subject=geophysics&rft_subject=petroleum exploration&rft_subject=AU-QLD&rft_subject=Published_External&rft.type=dataset&rft.language=English Access the data

Licence & Rights:

Open Licence view details
CC-BY

Creative Commons Attribution 4.0 International Licence
http://creativecommons.org/licenses/by/4.0

Creative Commons Attribution 4.0 International Licence

CC-BY

4.0

http://creativecommons.org/licenses/

WWW:LINK-1.0-http--link

Australian Government Security ClassificationSystem

https://www.protectivesecurity.gov.au/Pages/default.aspx

WWW:LINK-1.0-http--link

Access:

Open

Brief description

A reconnaissance seismic survey was made in the area of Quilpie and Et.omanga in south-western Queensland. Traverses crossed the Harkaway, Pinkilla, and Tallyabra Domes. Reflection horizons were correlated with horizons within the Mesozoic sediments, and one persistent reflection was correlated with a horizon near the top of the Palaeozoic sediments. A thickness of sediments of up to 15,000 ft, including up to 11,000 ft of Palaeozoic rocks, was indicated on the flanks of the Harkaway and Pinkilla Domes. Results were compared with existing gravity data. Suggestions of faulting are based on seismic and gravity evidence taken together and also on gravity evidence alone in locations not covered by the seismic work.

Lineage

Maintenance and Update Frequency: asNeeded
Statement: Geological reconnaissance work by Geosurveys Ltd, on behalf of L.H. Smart Oil Exploration Pty Ltd, has disclosed the presence of numerous well-exposed anticlines in the Quilpie/Eromanga area of south-west Queensland, most of which appear to have been unrecognised previously. A broad reconnaissance gravity survey was also made and there was generally good correlation between these surface structures and the observed Bouguer anomalies, suggesting that the structures continued at depth.^To investigate the area further, the Bureau of Mineral Resources carried out a seismic survey.

Issued: 1962

Data time period: 1959-08-01 to 1959-08-07

This dataset is part of a larger collection

Click to explore relationships graph

145,-26 145,-27 142,-27 142,-26 145,-26

143.5,-26.5

text: westlimit=142.0; southlimit=-27.0; eastlimit=145.0; northlimit=-26.0

Identifiers