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Yilgarn Semi Detailed merged magnetic grid geodetic

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Created 20/01/2025

Updated 20/01/2025

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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. This magnetic grid has a cell size of 0.00083 degrees (approximately 86m).The data are in nanoTesla (or nT). The data used to produce this grid was acquired in 1987 by the WA Government, and consisted of 392575 line-kilometres of data at line spacing between 100m and 400m, and 60m terrain clearance. The data has had a variable reduction to the pole applied to centre the magnetic anomaly over the magnetised body. The VRTP processing followed a differential reduction to pole calculation up to 5th order polynomial. Magnetic inclination and declination were derived from the IGRF-11 geomagnetic reference model using a data representative date and elevation representative of the survey.

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Title Yilgarn Semi Detailed merged magnetic grid geodetic
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/4b59f752-3b7a-4787-9476-2e58ecaed478
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 01/07/1987 - 25/04/2005
Geospatial Coverage {"type": "Polygon", "coordinates": [[[113.9996, -36.0], [125.9999, -36.0], [125.9999, -24.9996], [113.9996, -24.9996], [113.9996, -36.0]]]}
Data Portal data.gov.au