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Line 19: + + + − The figure below shows the 2-D MT model beneath the Angore-1 well and the base of the Darai Limestone as observed in the well.+ − − [[file:applying-magnetotellurics_fig16-6.png|thumb|{{figure number|16-6}}Drafted from data in Hoversten, 1992.]]
Magnetotellurics case history: rugged carbonate terrain (Highlands of Papua New Guinea) (view source)
Revision as of 15:39, 21 January 2014
, 15:39, 21 January 2014→Survey results
==Survey results==
==Survey results==
[[file:applying-magnetotellurics_fig16-6.png|left|thumb|{{figure number|1}}Drafted from data in Hoversten, 1992.]]
More than 2,500 MT sites have been acquired in Papua New Guinea by numerous companies involved in exploration in the region (Mills, personal communication, 1994). BP Exploration (Hoversten, 1992) acquired MT data over both the Angore anticline and the Hides anticline. The interpreted models from these two data sets provide depth estimates of the base of the Darai Limestone to within 10% of the measured depth in the Angore 1 well. In both cases, the seismic data aided the interpretation.
More than 2,500 MT sites have been acquired in Papua New Guinea by numerous companies involved in exploration in the region (Mills, personal communication, 1994). BP Exploration (Hoversten, 1992) acquired MT data over both the Angore anticline and the Hides anticline. The interpreted models from these two data sets provide depth estimates of the base of the Darai Limestone to within 10% of the measured depth in the Angore 1 well. In both cases, the seismic data aided the interpretation.
[[:file:applying-magnetotellurics_fig16-6.png|Figure 1]] shows the 2-D MT model beneath the Angore-1 well and the base of the Darai Limestone as observed in the well.
==See also==
==See also==