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 Colac-Geelong Gravity (P197131) contains a total of 2146 point data values acquired at a spacing between 400 and 900 metres. The data is located in VIC and were acquired in 1971, under project No. 197131 for Shell Development (Australia) 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 Mannum-Adelaide Pipeline Traverse, Gravity (P197143) contains a total of 44 point data values acquired at a spacing between 500 and 4000 metres. The data is located in SA and were acquired in 1971, under project No. 197143 for Department of Mines and Energy South Australia (SADME).

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 Alligator River Gravity (P197205) contains a total of 341 point data values acquired at a spacing of 500 metres. The data is located in NT and were acquired in 1972, under project No. 197205 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 Goulburn, Owen River Valleys, Gravity (P197206) contains a total of 977 point data values acquired at a spacing between 740 and 2000 metres. The data is located in NSW, VIC and were acquired in 1972, under project No. 197206 for Department of Mines (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 Uralla-Kentucky Gravity (P197248) contains a total of 132 point data values acquired at a spacing between 15 and 30 metres. The data is located in NSW and were acquired in 1972, under project No. 197248 for University of New England (UNE).

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 Bruny Islands Detailed Gravity (P197250) contains a total of 432 point data values acquired at a spacing between 200 and 800 metres. The data is located in TAS and were acquired in 1972, under project No. 197250 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 Anabama Fault Gravity (P197259) contains a total of 377 point data values acquired at a spacing between 150 and 800 metres. The data is located in SA and were acquired in 1972, under project No. 197259 for Department of Mines and Energy South Australia (SADME).

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 Yorke Peninsula Region Gravity 72E1 (P197261) contains a total of 125 point data values acquired at a spacing between 1500 and 1600 metres. The data is located in SA and were acquired in 1972, under project No. 197261 for Department of Mines and Energy South Australia (SADME).

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 Naracoorte Infill Gravity (P197260) contains a total of 29 point data values acquired at a spacing between 2500 and 4500 metres. The data is located in SA and were acquired in 1972, under project No. 197260 for Department of Mines and Energy South Australia (SADME).