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 Great Lake Region Gravity (P196250) contains a total of 223 point data values acquired at a spacing of 1250 metres. The data is located in TAS and were acquired in 1962, under project No. 196250 for University of Tasmania.

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 Rossarden Detailed Gravity (P197352) contains a total of 321 point data values acquired at a spacing between 17 and 175 metres. The data is located in TAS and were acquired in 1973, under project No. 197352 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 Soviet Pendulum Isogal Ties (P197499) contains a total of 1 point data values acquired at a spacing of None metres. The data is located in TAS and were acquired in 1974, under project No. 197499 for Bureau of Mineral Resources (BMR); USSR CRIGASC.

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 Helicopter Gravity Eastern Australia - Tasmania (P197304) contains a total of 19 point data values acquired at a spacing between 10000 and 21000 metres. The data is located in TAS and were acquired in 1973, under project No. 197304 for Wongela Geophysical Pty 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 Helicopter Gravity Eastern Australia - Tasmania (BMR7300) (P197303) contains a total of 1122 point data values acquired at a spacing between 6000 and 6250 metres. The data is located in TAS and were acquired in 1973, under project No. 197303 for Wongela Geophysical Pty 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 Isogal Tie Hobart K to Hobart T (P197530) contains a total of 1 point data values acquired at a spacing of None metres. The data is located in TAS and were acquired in 1975, under project No. 197530 for University of Tasmania.

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 Central Tasmania Gravity Survey, 2007 (P200751) contains a total of 1888 point data values acquired at a spacing between 500 and 7500 metres. The data is located in TAS and were acquired in 2007, under project No. 200751 for Great South Land Minerals.

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 Zeehan Gravity Survey, 2006 (P200671) contains a total of 3260 point data values acquired at a spacing between 10 and 100 metres. The data is located in TAS and were acquired in 2006, under project No. 200671 for Zeehan Zinc 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 East Central Tasmania Gravity (HINCH) (P196440) contains a total of 367 point data values acquired at a spacing between 500 and 2000 metres. The data is located in TAS and were acquired in 1964, under project No. 196440 for University of Tasmania.

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 Northwest Railway Gravity (P196353) contains a total of 104 point data values acquired at a spacing between 1000 and 5000 metres. The data is located in TAS and were acquired in 1963, under project No. 196353 for University of Tasmania.