Zobrazeno 1 - 10
of 357
pro vyhledávání: '"Douglas W. Oldenburg"'
Publikováno v:
Geophysics; Nov2014, Vol. 79 Issue 6, pX27-X33, 7p
Publikováno v:
Interpretation. 5:Y1-Y1
In Table 3, the color for R2 should have been blue and the color for R3 should have been yellow. The correct version of Table 3 appears below. View this table: Table 3. Petrophysical domains built from inversions of airborne geophysical data sets. He
Publikováno v:
GEOPHYSICS. 79:X32-X33
We thank Andre Revil for his interest in our paper (McMillan and Oldenburg, 2014) and for raising some concerns, and we would like to add a few comments in reply. Mr. Revil mentions in his discussion two assumptions that have been made in our paper.
Autor:
André Revil
Publikováno v:
GEOPHYSICS. 79:X27-X31
McMillan and Oldenburg (2014) develop a method for cooperatively inverting multiple electromagnetic data sets to produce a “consistent” 3D resistivity/conductivity model with improved resolution. Their data set includes airborne-time-domain elect
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Publikováno v:
Pure and Applied Geophysics. 179:2365-2381
Autor:
Lindsey J Heagy, Douglas W Oldenburg
SUMMARY Electromagnetic methods are increasingly being applied in settings with steel infrastructure. These include applications such as monitoring of CO2 sequestration or even assessing the integrity of a wellbore. In this paper, we examine the impa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a67236a6de893a495899e85ba8ede151
http://arxiv.org/abs/2211.14677
http://arxiv.org/abs/2211.14677
Publikováno v:
Engineering Geophysics ISBN: 9781003184676
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9c301862bc7fd1aec0aba1d577ffb07e
https://doi.org/10.1201/9781003184676-6
https://doi.org/10.1201/9781003184676-6
Publikováno v:
Pure and Applied Geophysics. 178:2171-2190
The gravity and magnetic data sets over a geothermal source are investigated to explore the geological features and geothermal system manifestations. The raw gravity data sets are firstly corrected for drift, latitude and free-air effects to obtain f
Publikováno v:
Interpretation. 8:SS47-SS62
We have carried out petrophysically and geologically guided inversions (PGIs) to jointly invert airborne and ground-based gravity data and airborne magnetic data to recover a quasi-geology model of the DO-27 kimberlite pipe in the Tli Kwi Cho (also r