1887
ASEG2012 - 22nd Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

Full Tensor Gravity Gradiometry (FTG) data measures the 5 independent tensor components, providing us with a measurement of the complete gravity field; standard visualisation techniques do not always allow us to extract the best from this dataset.

Tensor axis realignment allows us to visualise the data in an alternative reference frame, rather than the typical East-North-Down system used for gravity gradiometry which is chosen because it conforms to mapping conventions rather than for any geological reason.

With axis realignment, the coordinates are rotated about the z-axis, so we are effectively visualising the potential field from a different orientation. In doing this we highlight different geological trends which were not so prominently visualised in the typical END coordinate frame.

By using tensor axis realignment we are able to draw out further geological information from FTG data and hence produce a better interpretation of the dataset. Tensor axis realignment provides a way to visualise the threedimensionality of FTG data and gain more geological insight into the survey area.

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/content/journals/10.1071/ASEG2012ab239
2012-12-01
2026-01-17
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References

  1. Murphy, C.A. [2010] Recent developments with Air-FTG®: In R.J.L Lane (editor), Airborne Gravity 2010 – Abstracts from the ASEG-PESA Airborne Gravity 2010 Workshop: Published jointly by Geoscience Australia and the Geological Survey of New South Wales, Geoscience Australia Record 2010/23 and GSNW File GS2010/0457.
/content/journals/10.1071/ASEG2012ab239
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  • Article Type: Research Article
Keyword(s): 3D Gravity; Gravity Gradiometry; visualisation
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