Changes

==Survey results==

==Survey results==

[[file:applying-magnetotellurics_fig16-6.png|left|thumb|{{figure number|1}}Drafted from data in Hoversten, 1992.]]

[[file:applying-magnetotellurics_fig16-6.png|left|thumb|{{figure number|1}}2-D MT model beneath the Angore-1 well and the base of the Darai Limestone as observed in the well. Drafted from data in Hoversten.<ref name=Hoversten>Hoversten, G. M., 1996, Papua New Guinea MT: looking where seismic is blind: Geophysical Prospecting, vol. 44, p. 935-961.</ref>]]

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, 1996) 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.

[[: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.