Hi

Thanks for all the advice and references.

Dhananjay, the paper from Reid et al was helpful.  I hadn't considered
going back to those older papers by Nabighian, so I will check those out as
well.

Ed, the papers from Philips that I found had good examples of comparing
different methods and source types.  Specifically I found this one most
useful, for anyone that is interested: Locating magnetic contacts: a
comparison of the horizontal gradient, analytic signal, and local
wavenumber methods, SEG 2000.

Steve, the forward modelling approach sounds like a good way of testing the
results.  Some projects have so little information I was hoping to use
depth estimate methods to help construct forward models, but that sounds
like a good way of checking which method is most suitable.

I still haven't found very many papers specifically using gravity.  I did
try the horizontal gradient method with SI=0 for thin density sheet and the
HGM of the vertical derivative with SI=-1 for a vertical contact using the
USGS GX.  Does anyone use Euler for gravity grids?  What SI would you use
for a dipping or sub-vertical contact?  The paper by Reid says -1, but I
don't think I can set it to be less than 0






On Fri, May 1, 2015 at 11:55 AM, edcunion <[email protected]> <
[email protected]> wrote:

>   Some examples of usgs  mag-grav depth determination results are
> illustrated  from a handful of Jeff Phillips papers on these methods. These
> are available as pdfs from different web sources. I've used older manual
> graphical rule of thumb methods as crosschecks on these using a profile or
> two usually for larger aeromag datasets.
>
>
>
> Ed Cunion
>
>
>
> Sent from my T-Mobile 4G LTE device
>
>
>
>
>
> ------ Original message------
>
> *From: *Dhananjay Ravat
>
> *Date: *Fri, 5/1/2015 11:21 AM
>
> *To: *Geosoft Oasis montaj and Target;
>
> *Subject:*Re: [geonet] Depth to source methods
>
>
> Hi,  I presume all the potential field books have been looked into for
> methodological details and a lot of useful advice. This article below, and
> references therein, is a good place to start for the Euler method, if not
> already read.  For inclined contacts 2D analytical signal, carefully paying
> attention to Misac Nabighian’s (1972, 1974 Geophysics) use for thin sheets
> and trapezoids expressions and when to use anomaly and when to use its
> gradient will be helpful, and also the bell-shaped 2D analytic signal and
> their depth relationships will be helpful in determining parameters of
> interest. I know those papers have a lot of math, but I have found it very
> worthwhile struggling through that to understand what and why. Finally, in
> window based methods, there will always be a tradeoff between the size of
> the window, resolution, and noise in the data.  Similarly, noise in the
> data vs the use of methods that require higher order derivatives should be
> a consideration as I am sure you know.  I have found it useful to compare
> results from compatible methods as you are doing.   I hope this is useful.
> Best wishes, -tiku
>
> GEOPHYSICS, VOL. 79, NO. 4 (JULY-AUGUST 2014); P. J61–J66, 3 FIGS., 1
> TABLE. 10.1190/GEO2013-0235.1 The structural index in gravity and
> magnetic interpretation: Errors, uses, and abuses by Alan B. Reid1 and
> Jeffrey B. Thurston2
> _____________________________
> D. Ravat | Professor of Geophysics
> Earth & Environmental Sciences | Physics & Astronomy
> University of Kentucky
> 101 Slone Research Building | Lexington, KY  40506-0053
> fax: +1 859 323 1938
>
> Web:
> http://ees.as.uky.edu/users/drava2
> https://www.researchgate.net/profile/Dhananjay_Ravat/
> https://ees.as.uky.edu/gravity-magnetics-heat-flow-tectonics
> https://ees.as.uky.edu/near-surface-geophysics
> _____________________________
>
>
>
>
>
>
> On May 1, 2015, at 12:25 PM, Doug Perkin <[email protected]> <
> [email protected]> wrote:
>
> Hi
>
> I have been trying various source depth estimation methods for grids of
> potential field data and wanted to start a discussion on which methods tend
> to provide better solutions for gravity vs aeromag.  I am usually
> interested in sub vertical or dipping contacts, so for magnetics I have
> tried a structural index of 0 or 1 and for Gravity I have tried 0 and -1
> using the USGS special function depth analysis GX.  I have also tried Euler
> with various window sizes.
>
> The local wavenumber method using the USGS GX was interesting because it
> actually provides estimates of the structural index for various anomalies;
> however that method tended to give a lot more noise and was in places
> giving me a structural index of 3 when the RTP grid clearly did not look
> like a magnetic dipole source.
>
> Does anyone have experience with these depth estimation methods?  Which
> methods tend to give more reliable solutions for a vertical or dipping
> contact using aeromag?  And which methods tend to provide better solutions
> for a vertical or dipping contact using gravity?  Any advice or discussion
> on these methods would be much appreciated
>
> Regards,
> Doug
>
>
>
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