1887
ASEG2010 - 21st Geophysical Conference
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

A marine continuous seismic (CSP) profiling study and a resistivity study of vibrocore samples of shallow marine sands were undertaken in Jervis Bay, NSW, Australia, to characterise the seabed. The CSP study also included Crookhaven Bight, adjacent to Jervis Bay facing northeast to the ocean. The results of the CSP studies show variable geological conditions below the seabed, indicating very dense sands and variably weathered sandstones. The bedrock surface was also highly irregular in places suggesting cyclic erosional pulses under rapidly falling sea levels at various times in the past. Bedrock was found to form the seafloor in some locations and deeply incised paleochannels extending to -62 m below sea level in the Crookhaven Bight and bay entrance areas.

The sampled sands had very low magnetic susceptibilities, thus corroborating the visual impression of low clay content. However, a variety of grainsizes, grainshapes, colours and cohesions were noted. These factors, together with variations in inferred porosity, gave rise to a range of resistivities, which, when temperature corrected, plotted with some scatter about an appropriate Archie Equation curve. Resistivity values recorded ranged from ~ 1.0 to 0.8 Ω m (20°C) for the samples obtained from 11 sites.

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/content/journals/10.1081/22020586.2010.12041845
2010-12-01
2026-01-23
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References

  1. Albani, A.D., Carter, A.N. and Johnson, B.D., 1973, The bedrock topography of Jervis Bay, New South Wales: Oceanography of the South Pacific 1972, comp. R. Fraser, New Zealand Commision for UNESCO,Wellington, 1973, 179-184.
  2. Archie, G.E.,1942, The electrical resistivity log as an aid in determining some resevoir characteristics: Transactions AIME, 146, 54-62.
  3. Clark, D.A. and Emerson, D.W., 1991, Notes on rock magnetisation characteristics in applied geophysical studies: Exploration Geophysics, 22, 547-555.
  4. Emerson, D.W., 2000, Magnetic susceptibility insedimentary basin studies –some features of the Hawkesbury Sandstone: ASEG Preview, 87, 135-138.
  5. Jackson, P.D., Taylor Smith, D. and Stanford, P.N., 1978, Resistivity-porosity-particle shape relationships for marine sands: Geophysics, 43, 1250-1268.
  6. Taylor, G., 1972, Sedimentation in Jervis Bay: Proceedings of the Linnean Society of New South Wales, 96 (Part 4), 297-306.
  7. Taylor, G., Abell, R. and Paterson, I., 1995, Jervis Bay – a place of culture, scientific and educational value, in: Cho, Georges and Stoutjesdijk (editors), Canberra, ANPWS, 41-52.
  8. Vrbancich, J., 2009, An investigation of seawater and sediment depth using a prototype airborne electromagnetic instrumentation system – a case study in Broken Bay, Australia: Geophysical Prospecting, 57, 633-651.
  9. Whiteley, R.J. and Stewart, S.B., 2008, Case studies of shallow marine investigations in Australia with advanced underwater seismic refraction (USR): Exploration Geophysics, 39, 34-40.
/content/journals/10.1081/22020586.2010.12041845
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  • Article Type: Research Article
Keyword(s): bedrock topography; Jervis Bay.; marine seismic; sediment resistivity
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