1887

Abstract

Geophysical information, when spatially extensive, can be used to examine the relationships that may exist between geological classification schemes and their geophysical responses and/or properties. Geological geophysics essentially refers to any geophysical map that is based on, or classified according to, existing geological knowledge. Here the geological classification of subsurface values of conductivity, derived from airborne EM survey data, is assessed using survey data obtained across a small (36 x 22 km) area in the south of England. The characteristics of the highest frequency (closest to outcrop) conductivity distributions are examined in relation to two existing sedimentary bedrock classification schemes. Geological classifications of the data are found to explain over 75% of the variability in observed values. It is then demonstrated how the central moments and dispersion statistics of the distributions obtained can be used to predict the continuous near-surface conductivity distribution across a major area of southern England containing, as it does, a high population density and extensive infrastructure.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.20144364
2011-09-12
2024-04-20
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20144364
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error