The crustal structure of the Gulf of Papua and northwest Coral Sea
Interpretation of seismic refraction data from the southwestern coast of the Papuan Peninsula and the northwest Coral Sea gives consistent results using several inversion techniques. Sediments over the Papuan Plateau are 5 km thick; to the west and northwest they thicken to 10 km along the axes of the Moresby and southern Aure Troughs. Farther out into the Coral Sea, over the Eastern Plateau, they are 1 to 2 km thick. Beneath the sediments, a layer with a P-wave velocity of 6.07 km s^-1 was inferred over the region. It is underlain along the southern coastline of the peninsula by a lower crustal layer with a velocity of 6.9 km s^-1, which is probably also present under the Eastern Plateau. We cannot say whether the lower crustal layer also occurs offshore under the Moresby Trough, but it is not present under the Aure Trough in the north. Intervals where the velocity increases with depth are likely in the lower crust (> 17 km) under the peninsula, but we have insufficient data to say if they are present offshore. The Moho is 27 to 29 km deep along the southwestern coast of the peninsula. It shallows to 19 km under the Moresby Trough and deepens to 25 km under the Eastern Plateau. The crust is therefore continental under the Papuan Peninsula and Eastern Plateau and, excluding the sediments, oceanic under the Moresby Trough. We have examined several tectonic models for the region that imply different stress patterns at the time of formation of the Moresby Trough. We favour one in which northern Australia, the Eastern and Papuan Plateaus and the Papuan Peninsula once formed a continuous, continental crust. With the opening of the Coral Sea Basin, crustal thinning extended northwards along the axis of the Moresby Trough, probably into the Aure Trough. This model implies a regional tensional stress pattern at the time of formation.
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- Date (Publication)
- 1979-01-01T00:00:00
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- Geoscience Australia Persistent Identifier/https://pid.geoscience.gov.au/dataset/ga/81012
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Role Organisation / Individual Name Details Publisher Bureau of Mineral Resources, Geology and Geophysics
Canberra Author Drummond, B.J.
1 Author Collins, C.D.N.
2 Author Gibson, G.
3
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BMR Journal of Australian Geology and Geophysics
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4:4:341-351
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Product data repository: Various Formats
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GA Publication
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Journal
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marine
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AUS
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PNG
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- Australian and New Zealand Standard Research Classification (ANZSRC)
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Earth Sciences
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Published_External
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Creative Commons Attribution 4.0 International Licence
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CC-BY
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4.0
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Australian Government Security ClassificationSystem
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- 2018-11-01T00:00:00
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Journal article (pdf)
Journal article (pdf)
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pdf
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Australian Government Security ClassificationSystem
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- 2018-11-01T00:00:00
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urn:uuid/fae9173a-6fd1-71e4-e044-00144fdd4fa6
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GeoNetwork UUID
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Role Organisation / Individual Name Details Point of contact Commonwealth of Australia (Geoscience Australia)
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AGSO BMR Journal
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Geoscience Australia - short identifier for metadata record with
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- Date info (Revision)
- 2018-04-20T06:08:34
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- 2014-06-03T00:00:00
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AU/NZS ISO 19115-1:2014
Metadata standard
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ISO 19115-1:2014
Metadata standard
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ISO 19115-3
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Geoscience Australia Community Metadata Profile of ISO 19115-1:2014
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Version 2.0, September 2018
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Product catalogue