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 Clonagh Detailed Gravity Survey, Qld, 2004, CR47619. (P200445) contains a total of 48 point data values acquired at a spacing between 400 and 800 metres. The data is located in QLD and were acquired in 2004, under project No. 200445 for Minotaur Exploration Ltd.

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 Mt Isa Seismic (P200601) contains a total of 1610 point data values acquired at a spacing of 400 metres. The data is located in QLD and were acquired in 2006, under project No. 200601 for None.

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 Charleville-Adavale-Quilpie Gravity (P196406) contains a total of 125 point data values acquired at a spacing of 1609 metres. The data is located in QLD and were acquired in 1964, under project No. 196406 for Bureau of Mineral Resources (BMR).

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 Dobbyn Area Detail Gravity (P196407) contains a total of 104 point data values acquired at a spacing between 400 and 1000 metres. The data is located in QLD and were acquired in 1964, under project No. 196407 for Bureau of Mineral Resources (BMR).

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 Windorah Gravity (P196333) contains a total of 517 point data values acquired at a spacing between 804 and 2438 metres. The data is located in QLD and were acquired in 1963, under project No. 196333 for Alliance Oil Development NL.

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 Semi Detailed Gravity (P196712) contains a total of 2178 point data values acquired at a spacing of 100 metres. The data is located in QLD and were acquired in 1967, under project No. 196712 for Bureau of Mineral Resources (BMR).

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 Rockhampton Data (P197935) contains a total of 442 point data values acquired at a spacing of 450 metres. The data is located in QLD and were acquired in 1979, under project No. 197935 for None.

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 Georgina Basin Gravity Seismic (P197712) contains a total of 137 point data values acquired at a spacing of 500 metres. The data is located in NT, QLD and were acquired in 1977, under project No. 197712 for Bureau of Mineral Resources (BMR).

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 Cape York Complete Spherical Cap Bouguer First Vertical Derivative geodetic is the first vertical derivative of the complete spherical cap Bouguer anomaly grid for the Cape York Gravity Survey, Qld, 2009 (P200940). This gravity survey was acquired under the project No. 200940 for the geological survey of QLD. The grid has a cell size of 0.0075 degrees (approximately 820m). A Fast Fourier Transform (FFT) process was applied to the original grid to calculate the first vertical derivative grid. A total of 9244 gravity stations at 4000m spacing were acquired to produce this grid.

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 Cape York Gravity Survey, Qld, 2009 (P200940) contains a total of 9244 point data values acquired at a spacing of 4000 metres. The data is located in QLD and were acquired in 2009, under project No. 200940 for Geological Survey of Queensland (GSQ).