From Geoscience Australia

Gravity evidence for a major crustal fracture in eastern Australia

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Created 13/01/2025

Updated 13/01/2025

Gravity data are presented for 220 sites covering 180 000 square kilometres in the Prince Charles Mountains area of eastern Antarctica. Bouguer anomalies range from +60 m Gal over the Amery Ice Shelf (near sea level) to -120 m Gal at altitudes above 2000 m on the Antarctic ice cap. Bouguer anomalies correlate with the mass per unit area above sea level in the relation expected for a region in isostatic equilibrium. Smoothed free air anomalies range from +60 to -60 mGal. North-south trending anomalies over the Lambert Glacier and Amery Ice Shelf are thought to be due to a major fault along the Lambert Glacier, and a rift structure under the Amery Ice Shelf. To the west of these structures the free air anomalies trend mainly east-west.

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Field Value
Title Gravity evidence for a major crustal fracture in eastern Australia
Language eng
Licence notspecified
Landing Page https://devweb.dga.links.com.au/data/dataset/d980b170-110c-452f-b8c2-d012bcf6244e
Contact Point
Geoscience Australia
clientservices@ga.gov.au
Reference Period 20/04/2018
Geospatial Coverage {"type": "Polygon", "coordinates": [[[60.0, -75.0], [76.0, -75.0], [76.0, -67.0], [60.0, -67.0], [60.0, -75.0]]]}
Data Portal data.gov.au

Data Source

This dataset was originally found on data.gov.au "Gravity evidence for a major crustal fracture in eastern Australia". Please visit the source to access the original metadata of the dataset:
https://devweb.dga.links.com.au/data/dataset/gravity-evidence-for-a-major-crustal-fracture-in-eastern-australia

No duplicate datasets found.