1887
Volume 29, Issue 3-4
  • ISSN: 0812-3985
  • E-ISSN: 1834-7533

Abstract

The gamma-ray spectrometric data over an exposed granite batholith contains detailed information on its structure and composition. The information is poorly displayed in the conventional red-green-blue or hue-saturation-intensity colour-space images. Variation diagrams can be prepared showing the relationship between K, Th and U, and the data can be displayed as a map of distance along the average variation path, and deviation of the observed concentrations from this average variation path. Alternatively, the rocks can be separated into subdivisions of granite types, and these types mapped using separate classification layers.

For the Mount Edgar Batholith, gamma-ray spectrometry results are compared with the results from other techniques – rock sample geochemistry, petrography, air photo interpretation, field observations, structural studies, magnetic anomalies, and Landsat-5 Thematic Mapper data enhanced for geology. In this outcropping batholith the spectrometric data are thought to be superior technique in determining batholith structure and compositional variation, because of it has greater resolution than field mapping and rock sample geochemistry, and because of its tie to rock geochemistry that is lacking in magnetic anomalies.

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/content/journals/10.1071/EG998643
1998-09-01
2026-01-15
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References

  1. Blockley, J.G., 1980, The tin deposits of Western Australia with special reference to the associated granites: Geol. Surv. WA Min. Res. Bull. 12, 1–184.
  2. Collins, W.J., 1983, Geological evolution of an Archaean batholith. PhD Thesis, University of La Trobe, Melbourne (unpubl.).
  3. Collins, W.J., 1989, Polydiapirism of the Archaean Mount Edgar Batholith, Pilbara Block, Western Australia: Precambrian Res. 43, 41–62.
  4. Collins, W.J. and Grey, C.M., 1990, Rb-Sr isotopic systematics of an Archaean granite-gneiss terrain: the Mount Edgar Batholith, Pilbara Block, Western Australia: Austral. J. Earth Sci. 37, 9–22.
  5. Davy, R. and Lewis, J.D., 1986, The Mount Edgar Batholith, Pilbara area, Western Australia: geochemistry and petrography: Geol. Surv. WA Rep. 17, 1–43.
  6. Glikson, A.Y., 1997, Mineral mapping in the north Pilbara Craton: a directed-principal-components-of-band-ratios method for correlating Landsat-5 Thematic Mapper spectral data with geology: AGSO Res. Newsletter 26, 1–4.
  7. Hickman, A.H., 1983, Geology of the Pilbara Block and its environs: Geol. Surv. WA Bull. 127, 1–268
  8. Milligan, PR. and Gunn, P.J., 1997, Enhancement and presentation of airborne geophysical data: AGSO J. Austral. Geol. Geophy. 17, 63–75.
  9. Richardson, L.M., 1997, Marble Bar airborne geophysical survey, 1996 - operations report: Austr. Geol. Surv. Org. Record 1997/63, 1–57.
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  • Article Type: Research Article
Keyword(s): gamma-ray; granite; magnetic anomaly; mapping; spectrometry

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