Hi everyone, and special thanx to Ken for all the Calgary Meeting updates. 
While SEG-members will be busy giving each other esteemed awards, Crebs will 
hopefully be discovering orebodies <grin>; to that:

Interpretation geophysicists should be aware that Fugro's helicopter 
electromagnetic (HEM) systems now normalize the coplanar-coil signal response 
DIFFERENTLY than the Dighem systems prior to 1999. The new normalization 
process essentially doubles the response magnitude (in units of ppm); and 
apparently is normalized similar to the previous High-Sense, Aerodat, and 
SIAL HEM-systems. The coaxial-coil normalization remains the same as earlier 
pre-1999 systems.

This is very important to interpretation geophysicists who rely on 
coaxial-to-coplanar (@ "nearby" frequencies) response-ratios to help 
discriminate conductive ore-geometries from culture and graphitic conductors. 
Whereas spherical-shaped ore-geometries prior to 1999 yielded a Dighem 
theoretical-ratio of 1/4 ; the new Fugro coplanar normalization yields a 
ratio of 1/8! (Here's a real example, the Voisey's Bay "Ovoid" orebody 
yielded a coaxial-to-coplanar ratio of about 2/7 (@ near 900-hertz) when 
surveyed by Dighem for me in 1995; therefore, under the new Fugro 
normalization its ratio would be 1/7.)

This could also be important when comparing older Dighem surveys with newer 
Fugro-acquired data. If you use older Dighem characteristic curves for 
profile interpretations, make a note of the change. Processing geophysicists 
should also be aware of this normalization change; so fix your 
filtering/modeling/inversion algorithms accordingly.

Good Prospecting,
Terry J. Crebs
formerly, Chief Geophysicist, Diamond Fields Resources, Inc.
Lakewood, CO  USA
http://www.crebs.com

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