Hello,
Thanks for the suggestions.
Best regards,
Ana

De: Gerry Connard <[email protected]> [mailto:[email protected]]
Enviada: segunda-feira, 23 de Novembro de 2015 18:44
Para: Geosoft Oasis montaj and Target
Assunto: RE: [geonet] Potential field data modeling in GM-SYS

As Ed points out, using RTP where remanence is present can cause problems.  In 
general it is better to use TMI data.  GM-SYS does not apply a correction to 
the TMI data but uses the external field parameters to calculate the model 
response in the presence of that external field.

The only exception to this recommendation is the case where the external field 
varies significantly over your model (for example a long profile near the 
magnetic pole).  In this case you may be better off doing a variable RTP before 
trying to model because GM-SYS only allows you to enter 1 definition for the 
external field.

Most modern aeromag surveys remove the variations in the IGRF/DGRF from the 
final delivered data.  They typically subtract the appropriate field based on 
the location & elevation of each measured point.  Alternatively, the 
contractors compute a grid of IGRF values across the survey area and subtract 
that from the observed data.

The ‘total field” magnetic anomaly is a scalar value derived by taking the dot 
product of the observed vector magnetic field with the regional field (i.e. the 
IGRF) at that point.  See Blakely (1995, p178-179). GM-SYS 2D and 3D need the 
regional field strength value and direction to calculate the total field 
anomaly.

Blakely, R.J., 1995, Potential Theory in Gravity & Magnetic Applications: 
Cambridge University Press, pp.441.

Gerry

From: edcunion <[email protected]<mailto:[email protected]>> 
[mailto:[email protected]]
Sent: Monday, November 23, 2015 9:19 AM
To: Geosoft Oasis montaj and Target
Subject: Re: [geonet] Potential field data modeling in GM-SYS

On your latter general remanence query, the RTP filtered product can show 
affects when remanence is present, the affects can be exacerbated at low 
magnetic latitudes. Comparing the TMI and RTP with the analytic signal or its 
individual derivative components (dX, dY, dZ)  for your data can add some 
insight.

The ASVI (analytic signal of the vertical integral, in Macleod et al 1993) can 
also be tried and compared, the reference is quoted below and outlines this 
method-

"Macleod, I.N., Vieira, S., Chaves, A.C., 1993; Analytic signal and reduction 
to the pole in the interpretation of total magnetic field data at low magnetic 
latitudes, Proceedings of the third international congress of the Brazilian 
Society of Geophysicists."


Ed




On Monday, November 23, 2015 9:17 AM, author.nameemail 
<[email protected]<mailto:[email protected]>> wrote:

Hello,
I want to clarify some doubts about potential field data modeling in GM-SYS. I 
can use the TMI or the RTP anomaly when I am modeling magnetic data. But when I 
am modeling simultaneously magnetic and gravity data is better to use the 
gravity and reduced to the pole magnetic anomaly? Because the dipolar effect is 
removed and magnetic anomalies are transformed to monopolar like the gravity 
anomaly. Ideally what anomaly should I use in this case?
Or does the GMSYS apply some correction to the TMI data, because when I create 
a gmsys model I have to define the magnetic field parameters (magnitude, 
inclination and declination) at the measurement location?
Other question is related to the presence of remanance magnetization. When 
remanent magnetization is present is better to use the TMI data and not the RTP 
anomaly? Or I can use other derivative grid like the analytical signal?
Best regards,
Ana

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