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 Eromanga Gravity (P198113) contains a total of 69 point data values acquired at a spacing of 500 metres. The data is located in QLD and were acquired in 1981, under project No. 198113 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 Seismic Gravity Trav Central Eromanga Basin Trav6-2 (P198114) contains a total of 77 point data values acquired at a spacing of 650 metres. The data is located in QLD and were acquired in 1981, under project No. 198114 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 Seismic Gravity Trav Central Eromanga Trav 10 (P198118) contains a total of 145 point data values acquired at a spacing of 650 metres. The data is located in QLD and were acquired in 1981, under project No. 198118 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 Seismic Gravity Data Central Eromanga Basin Trav1-9 (P198117) contains a total of 164 point data values acquired at a spacing of 500 metres. The data is located in QLD and were acquired in 1981, under project No. 198117 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 Seismic Gravity Trav Central Eromanga Basin Trav 12 (P198119) contains a total of 48 point data values acquired at a spacing of 650 metres. The data is located in QLD and were acquired in 1981, under project No. 198119 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 Bowen Surat Gravity Complete Bouguer Anomaly is a complete Bouguer anomaly grid for the Bowen Surat (P200540). This gravity survey was acquired under the project No. 200540 for the geological survey of QLD. The grid has a cell size of 0.00764 degrees (approximately 800m). The data are given in units of um/s^2, also known as 'gravity units', or gu. A total of 4977 gravity stations 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 Naraku EPM 12660 CR40038 (P200442) contains a total of 293 point data values acquired at a spacing between 200 and 400 metres. The data is located in QLD and were acquired in 2004, under project No. 200442 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 Clonagh Detailed Gravity Survey, Qld, 2004, EPM14292, CR39758. (P200443) contains a total of 403 point data values acquired at a spacing between 200 and 800 metres. The data is located in QLD and were acquired in 2004, under project No. 200443 for Red Metal 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 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 Isa Georgetown (P200140) contains a total of 5236 point data values acquired at a spacing of 4000 metres. The data is located in QLD and were acquired in 2001, under project No. 200140 for Department of Minerals and Energy (Queensland).