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Exploration Geophysics Exploration Geophysics Society
Journal of the Australian Society of Exploration Geophysicists
Exploration Geophysics

Exploration Geophysics

Volume 43 Number 2 2012


We show the application of simulated annealing to optimise our estimation of the parameters in the common reflection surface (CRS) stack method. This approach using numerically modelled data and multichannel marine seismic data around the Median Tectonic Line in Japan provides a clear seismic profile with a high signal-to-noise ratio.


In this study, we developed a forward modelling algorithm with the staggered-grid finite-difference method. The elastic wave propagation in 2D tilted transversely isotropic media is well simulated using this algorithm. We also implement convolutional perfectly matched layer absorbing boundaries in our algorithm in order to handle the artificial boundary reflection efficiently.

EG10015An enhancement of the formation factor parameters ‘a’ and ‘m’

Walid M. Mabrouk, Khalid S. Soliman and Mohamed A. Tawfic
pp. 87-94

The use of incorrect values of the formation constants a (tortuosity factor) and m (cementation exponent) in Archie’s water saturation equation can result in the overlooking of potential producible zones. This work illustrates a simple method of calculating a and m that is dependent on sonic transit time and bulk density, and on knowing one cementation exponent value from core measurements.

EG11044 3D inversion of SPECTREM and ZTEM airborne electromagnetic data from the Pebble Cu–Au–Mo porphyry deposit, Alaska

Pascal Pare, Alexander V. Gribenko, Leif H. Cox, Martin Čuma, Glenn A. Wilson, Michael S. Zhdanov, Jean Legault, Jaco Smit and Louis Polome
pp. 104-115

This case study compares 3D inversion results from SPECTREM 2000 fixed-wing time-domain airborne electromagnetic (AEM) and ZTEM airborne audio-frequency magnetics (AFMAG) systems flown over the Pebble Cu–Au–Mo porphyry deposit in south-western Alaska. Both 3D inversions recover conductors coincident with alteration associated with both Pebble East and Pebble West.


Network extraction is a routine applied to magnetic data to identify lineaments (e.g. faults and dykes). When these extracted lineaments are used in conjunction with existing geophysical and geological data, vectors for mineral potential may be identified. Network extraction was successfully applied to an aeromagnetic data set from Northwestern Canada.


The polarimetric borehole radar has the ability to characterise subsurface fractures. Nine fracture sets were characterised into four category fractures depending on polarimetric analysis of alpha, entropy and anisotropy decomposition. Validation of these results was implemented by numerical simulation for a synthesised fractures property using the Finite Difference Time Domain method.