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 Terang-Portland Gravity (P196936) contains a total of 2956 point data values acquired at a spacing between 400 and 1000 metres. The data is located in VIC and were acquired in 1969, under project No. 196936 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 Torquay Gravity (P196948) contains a total of 410 point data values acquired at a spacing between 300 and 1000 metres. The data is located in VIC and were acquired in 1969, under project No. 196948 for Geosurveys 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 Casterton Gravity (P197035) contains a total of 1138 point data values acquired at a spacing between 250 and 450 metres. The data is located in VIC and were acquired in 1970, under project No. 197035 for Planet Explor Co P/L.

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 Eildon Gravity (P197048) contains a total of 394 point data values acquired at a spacing between 250 and 1500 metres. The data is located in VIC and were acquired in 1970, under project No. 197048 for University of Melbourne.

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 BMR Soviet Australia Calibration Line (P197390) contains a total of 31 point data values acquired at a spacing of None metres. The data is located in ACT, NSW, NT, QLD, SA, TAS, VIC, WA and were acquired in 1973, under project No. 197390 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 Western Port Sunkland Victoria, Gravity (P197430) contains a total of 741 point data values acquired at a spacing of 805 metres. The data is located in VIC and were acquired in 1974, under project No. 197430 for University of Melbourne.

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 Penshurst Minhamite Detailed Gravity Survey EL4604 EL4579, Vic, 2005 (P200533) contains a total of 2807 point data values acquired at a spacing between 100 and 6500 metres. The data is located in VIC and were acquired in 2005, under project No. 200533 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 Raywood Ground Gravity Survey, Bendigo 2004, Vic EL 4661, EL4525 (P200430) contains a total of 194 point data values acquired at a spacing between 50 and 750 metres. The data is located in VIC and were acquired in 2004, under project No. 200430 for Lach Drummond Resources Ltd; Providence old and Minerals 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 Foster Gravity Traverses, Warragul, EL4810, EL3706, 2004 Vic (P200432) contains a total of 1068 point data values acquired at a spacing between 25 and 500 metres. The data is located in VIC and were acquired in 2004, under project No. 200432 for Sedimentary Holdings Ltd.