1887
2nd Australasian Exploration Geoscience Conference: Data to Discovery
  • ISSN: 2202-0586
  • E-ISSN:

Abstract

Summary

This study is part of the groundwater investigations of the Ord Bonaparte plains in the East Kimberley region of Western Australia. A key project aim is to establish a spatial hydrostratigraphic framework to better understand the hydrogeology.

To achieve this, AEM data, inverted using 1D SELMA model, were produced as conductivity sections and elevation grids. Interpretation of the AEM data, in conjunction with lithostratigraphic information from three petroleum wells and seven project bores, aided the mapping of hydrostratigraphic units of the Devonian to Permian sequence of the Bonaparte Basin. Mapping results show that the Carboniferous Weaber and Kushill Groups are dipping to the east-northeast and contain laterally continuous stacked aquifers. Within the strata, resistive signatures are associated with sandstone aquifers, slight to moderate conductors are mapped as fine textured aquitard, or as interbedded fine to coarse textured sediment forming semi-confining layers.

A water table elevation map was constructed using surface NMR water content profile and machine learning approach to extrapolate across the study area. Using Archie’s Law, groundwater conductivity was predicted from AEM conductivity and porosity derived from borehole NMR measurements.

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/content/journals/10.1080/22020586.2019.12073171
2019-12-01
2026-01-16
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References

  1. Archie, G. E. (1950). Introduction to petrophysics of reservoir rocks. AAPG Bulletin 34(5), 943–961. doi: 10.1306/3d933f62-16b1-11d7-8645000102c1865d.
  2. Auken, E., Christiansen, A. V., Jacobsen, B. H., Foged, N., and Sørensen, K. I., (2005), Piecewise 1D Laterally Constrained Inversion of resistivity data: Geophysical Prospecting, 53, 497–506.
  3. Auken, E., Christiansen, A.V., Kirkegaard, C., Fiandaca, G., Schamper, C., Behroozmand, A.A., Binley, A., Nielsen, E., Effersø, F., Christensen, N.B. and Sørensen, K., 2015. An overview of a highly versatile forward and stable inverse algorithm for airborne, ground-based and borehole electromagnetic and electric data. Exploration Geophysics, 46(3), pp.223-235.
  4. Christensen, N.B., (2016a). Strictly horizontal lateral parameter correlation for 1D inverse modelling of large data sets. Near Surface Geophysics, 14, 391-399. doi: 10.3997/1873-0604.2016028.
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  6. Gorter, J. D., Jones, P. J., Nicoll, R. S. and Golding, C. J. (2005). A reappraisal of the Carboniferous stratigraphy and the petroleum potential of the southeastern Bonaparte Basin (Petrel Sub-basin), northwestern Australia. APPEA Journal 45, 275-294.
  7. Lawrie, K., Symington, N., Tan, K., Christensen, N.B., Halas, L., Harris-Pascal, C., McPherson, A., Cathro, D. and Grunewald, E., 2018. Using AEM and GMR Methods for Non-Invasive, Rapid Reconnaissance Mapping and Characterisation of Groundwater Systems in the Kimberley Region, Northern Australia. ASEG Extended Abstracts, 2018(1), pp.1-1.
  8. Mory, A. J. and Beere, G. M. (1988). Geology of the onshore Bonaparte and Ord basins in Western Australia. Bulletin 134. Perth: Geological Survey of Western Australia. 179 p.
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  • Article Type: Research Article
Keyword(s): AEM; Bonaparte; groundwater; hydrostratigraphy; NMR
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