Authors / CoAuthors
Nakamura, A.
Abstract
This image is derived from gravity observations stored in the Australian National Gravity Database (ANGD) as at February 2016 as well as data from the 2013 New South Wales Riverina gravity survey. Out of the approximately 1.8 million gravity observations 1,371,998 gravity stations in the ANGD together with 19,558 stations from the Riverina survey were used to generate this image. The image shows isostatic residual gravity anomalies over onshore continental Australia. The data used in this image has been acquired by the Commonwealth, State and Territory Governments, the mining and exploration industry, universities and research organisations from the 1940's to the present day. The isostatic corrections were based on the assumption that topographic loads are compensated at depth by crustal roots following the Airy-Heiskanen isostatic principle. A crustal density of 2670 kg/m3 was used for the isostatic correction, with an assumed density contrast between the crust and mantle of 400 kg/m3. An initial average depth to Moho at sea level of 37 km was used in the calculation. The isostatic corrections were then applied to the Complete Bouguer Gravity Anomaly Grid of Onshore Australia 2016 to produce the isostatic residual gravity anomaly grid. The Isostatic Residual Gravity Anomaly Grid of Onshore Australia 2016 has been image enhanced and displayed as a hue-saturation-intensity (HSI) image with sun shading from the northeast to create this product.
Product Type
dataset
eCat Id
101106
Contact for the resource
Owner
Cnr Jerrabomberra Ave and Hindmarsh Drive
Symonston
ACT
2609
Australia
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Text
Publisher
Cnr Jerrabomberra Ave and Hindmarsh Drive
Symonston
ACT
2609
Australia
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Text
Author
Cnr Jerrabomberra Ave and Hindmarsh Drive
Symonston
ACT
2609
Australia
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia
Text
Digital Object Identifier
Keywords
- ( Theme )
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- gravity
- ( Theme )
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- isostatic residual
- ( Theme )
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- isostasy
- ( Theme )
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- National dataset
- ( Theme )
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- Gravity Digital Data
- ( Theme )
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- HSI
- ( Theme )
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- isostatic correction
- ( Theme )
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- isostatic anomaly
- Australian and New Zealand Standard Research Classification: Fields of Research
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- Earth Sciences
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- Published_External
Publication Date
2016-08-11T00:00:00
Creation Date
2016-07-21T00:00:00
Security Constraints
Legal Constraints
Status
Purpose
Maintenance Information
asNeeded
Topic Category
geoscientificInformation
Series Information
Lineage
This image is derived from gravity observations stored in the Australian National Gravity Database (ANGD) as at February 2016 as well as data from the 2013 New South Wales Riverina gravity survey. The data used to produce this image was the Isostatic Residual Gravity Anomaly Grid of Onshore Australia 2016. The isostatic residual anomaly grid has been image enhanced and displayed as a hue-saturation-intensity (HSI) image with sun shading from the northeast. Out of the approximately 1.8 million gravity observations 1,371,998 gravity stations in the ANGD together with 19,558 stations from the Riverina survey were used to generate this image. The image shows isostatic residual gravity anomalies over onshore continental Australia. The data used in this image has been acquired by the Commonwealth, State and Territory Governments, the mining and exploration industry, universities and research organisations from the 1940¿s to the present day. Continental Australia has a base coverage of 11 kilometres, with South Australia, Tasmania and part of New South Wales covered with gravity stations at a spacing of 7 kilometres. Victoria has station coverage of approximately 1.5 kilometres. Federal, State and Territory Government initiatives have systematically infilled at a station spacing of 2 to 4 kilometres to improve coverage in areas of scientific or economic interest. Other areas of detailed coverage have been surveyed by private companies for exploration purposes. Only open file data held in the ANGD at February 2016 were used in the creation of the grid. The 2013 Riverina survey was added to the gridding process as this survey was not in the ANGD at the time. The depth to mantle model and subsequent isostatic corrections were calculated using a modified version of the USGS program AIRYROOT (Simpson et al., 1983) provided by Intrepid Geophysics (1). The 2009 Bathymetry and Topography Grid (Whiteway, 2009) was used to calculate the depth to Mohorovi¿i¿ discontinuity (Moho) following the Airy-Heiskanen crustal root model. The bathymetry and topography grid was subsampled to 1 km cell size and then low pass filtered to remove spatial wavelengths greater than 50 km. A crustal density of 2670 kg/m3 was used for the isostatic correction, with an assumed density contrast between the crust and mantle of 400 kg/m3. An initial average depth to Moho at sea level of 37 km was used in the calculation. This was derived from refraction and wide-angle reflection seismic experiments and receiver function analyses around Australia (Goncharov et al., 2007). The isostatic corrections were then applied to the Complete Bouguer Gravity Anomaly Grid of Onshore Australia 2016 to produce the isostatic residual gravity anomaly grid. This grid was image enhanced and displayed as a hue-saturation-intensity (HSI) image with sun shading from the northeast to create this product. References: 1 http://www.intrepid-geophysics.com Goncharov, A., Deighton, I., Tischer, M. and Collins, C., 2007. Crustal thickness in Australia: where, how and what for? ASEG Extended Abstracts, 2007, 1-4, ASEG 2007 19th Geophysical Conference. Simpson, R.W., Jachens, R.C. and Blakely, R.J., 1983. AIRYROOT: A FORTRAN program for calculating the gravitational attraction of an Airy isostatic root out to 166.7 km. US Geological Survey Open File Report 83-883. Whiteway, T. G., 2009. Australian bathymetry and topograhy grid. Geoscience Australia, Canberra. http://dx.doi.org/10.4225/25/53D99B6581B9A
Parent Information
Extents
[-43.9, -10, 112.5, 154]
Reference System
GDA94 (EPSG:4283) GDA94 / Geoscience Australia Lambert (EPSG:3112)
Spatial Resolution
Service Information
Associations
Source Information