Total magnetic intensity (TMI) data measures variations in the intensity of the Earth's magnetic field caused by the contrasting content of rock-forming minerals in the Earth crust. Magnetic anomalies can be either positive (field stronger than normal) or negative (field weaker) depending on the susceptibility of the rock. The data 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. These line dataset from the Murrindal, Vic, 1996 VIMP Survey (GSV3060) survey were acquired in 1995 by the VIC Government, and consisted of 15589 line-kilometres of data at 200m line spacing and 80m terrain clearance. To constrain long wavelengths in the data, an independent data set, the Australia-wide Airborne Geophysical Survey (AWAGS) airborne magnetic data, was used to control the base levels of the survey data. This survey data is essentially levelled to AWAGS.

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 Meelera Rockhole B Gravity (P198184) contains a total of 170 point data values acquired at a spacing of 200 metres. The data is located in SA and were acquired in 1981, under project No. 198184 for Afmeco 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 Seismic Gravity Trav Central Eromanga Basin Trav 6-2 (P198204) contains a total of 174 point data values acquired at a spacing of 650 metres. The data is located in QLD and were acquired in 1982, under project No. 198204 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 Trav 10 (P198210) contains a total of 244 point data values acquired at a spacing between 100 and 700 metres. The data is located in QLD and were acquired in 1982, under project No. 198210 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 Wanna Mason Detailed Gravity (P198233) contains a total of 310 point data values acquired at a spacing between 1000 and 6000 metres. The data is located in WA and were acquired in 1982, under project No. 198233 for CRA Exploration 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 Cahuna-Mitiamo Northern Plains, Victoria Gravity (P198241) contains a total of 369 point data values acquired at a spacing between 400 and 2500 metres. The data is located in VIC and were acquired in 1982, under project No. 198241 for Department of Minerals and Energy (Victoria).

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 Ballarat - St Arnaud Region Gravity (P198244) contains a total of 1633 point data values acquired at a spacing between 100 and 400 metres. The data is located in VIC and were acquired in 1982, under project No. 198244 for Department of Minerals and Energy (Victoria).

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 Balook Dome Warragul Gravity (P198246) contains a total of 630 point data values acquired at a spacing of 500 metres. The data is located in VIC and were acquired in 1982, under project No. 198246 for Geological Survey of Victoria (GSV).

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 Blackall Gravity on the Auberg Seismic Lines (P198248) contains a total of 401 point data values acquired at a spacing of 420 metres. The data is located in QLD and were acquired in 1982, under project No. 198248 for Anglo Australian Resources 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 East Midlands, St Helens Micro Detailed Gravity Eastern Part (P198251) contains a total of 982 point data values acquired at a spacing between 100 and 1000 metres. The data is located in TAS and were acquired in 1982, under project No. 198251 for Mineral Resources Tasmania (MRT).