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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Birrindudu NT Detailed Gravity Survey (P200580) contains a total of 3729 point data values acquired at a spacing of 2000 metres. The data is located in NT and were acquired in 2005, under project No. 200580 for Geoscience Australia; Northern Territory of Australia (Northern Territory Geological Survey).

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Coober Pedy Seismic, Gravity (P197087) contains a total of 149 point data values acquired at a spacing of 375 metres. The data is located in SA and were acquired in 1970, under project No. 197087 for Department of Mines and Energy South Australia (SADME).

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Nucha Gravity (P196530) contains a total of 400 point data values acquired at a spacing of 1609 metres. The data is located in NSW and were acquired in 1965, under project No. 196530 for Planet Explor Co P/L.

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Gravity Along Boulia Seismic Line Extension, 2015 (P201541) contains a total of 307 point data values acquired at a spacing of 400 metres. The data is located in QLD and were acquired in 2015, under project No. 201541 for Geoscience Australia.

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Lone Hill Seismic, Gravity (P196938) contains a total of 131 point data values acquired at a spacing of 480 metres. The data is located in NT and were acquired in 1969, under project No. 196938 for Australian Aquitaine Petroleum Pty Ltd.

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    Gravity data measure small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This North Perth Gingin Brook Gravity Spherical Cap Bouger Anomaly 267GU Geodetic p201360.ers is a complete Bouguer anomaly grid for the North Perth Gingin Brook Gravity Survey, 2013 (P201360) survey. This gravity survey was acquired under the project No. 201360 for the geological survey of WA. The grid has a cell size of 0.00363 degrees (approximately 374m). The data are given in units of um/s^2, also known as 'gravity units', or gu. A total of 1236 gravity stations were acquired to produce this grid.

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Wyloo Geochem-Gravity (P199861) contains a total of 1245 point data values acquired at a spacing of 4000 metres. The data is located in WA and were acquired in 1998, under project No. 199861 for Australian Geological Survey Organisation (AGSO); Geological Survey of Western Australia (GSWA).

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This Canegrass Low Region Gravity (P197565) contains a total of 34 point data values acquired at a spacing between 6500 and 7500 metres. The data is located in SA and were acquired in 1975, under project No. 197565 for Department of Mines and Energy South Australia (SADME).

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    The radiometric, or gamma-ray spectrometric method, measures the natural variations in the gamma-rays detected near the Earth's surface as the result of the natural radioactive decay of potassium (K), uranium (U) and thorium (Th). The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. The terrestrial dose rate grid is derived as a linear combination of the filtered K, U and Th grids. A low pass filter is applied to this grid to generate the filtered terrestrial dose rate grid. This GSWA North Canning 4 Lagrange Munro 2010 Doserate Grid Geodetic has a cell size of 0.00083 degrees (approximately 90m) and shows the terrestrial dose rate of the Lagrange-Munro, WA, 2010 (North Canning 4). The data used to produce this grid was acquired in 2010 by the WA Government, and consisted of 103921 line-kilometres of data at 400m line spacing and 60m terrain clearance.

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    Gravity data measures small changes in gravity due to changes in the density of rocks beneath the Earth's surface. The data collected are processed via standard methods to ensure the response recorded is that due only to the rocks in the ground. The results produce datasets that can be interpreted to reveal the geological structure of the sub-surface. The processed data is checked for quality by GA geophysicists to ensure that the final data released by GA are fit-for-purpose. This SA Detailed Gravity Survey 94E8 (P199458) contains a total of 1279 point data values acquired at a spacing of 200 metres. The data is located in SA and were acquired in 1994, under project No. 199458 for None.