1989
DOI: 10.3997/1365-2397.1989027
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Case histories of LOTEM surveys in hydrocarbon prospective area

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Cited by 45 publications
(11 citation statements)
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“…While not successful for this survey, it is a useful tool in workflows when honouring multiple data sets is key to a successful interpretation. The workflow pioneered in Western Australia was further substantiated in test surveys (Strack et al, 1989) and feasibility studies (Strack, 1992), an example of which is shown in Figure 4. The figure illustrated how geometric constraints are needed for CSEM interpretation and that indeed the electric fields are biased toward resistors and the magnetic fields are biased towards conductors.…”
Section: Discussionmentioning
confidence: 96%
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“…While not successful for this survey, it is a useful tool in workflows when honouring multiple data sets is key to a successful interpretation. The workflow pioneered in Western Australia was further substantiated in test surveys (Strack et al, 1989) and feasibility studies (Strack, 1992), an example of which is shown in Figure 4. The figure illustrated how geometric constraints are needed for CSEM interpretation and that indeed the electric fields are biased toward resistors and the magnetic fields are biased towards conductors.…”
Section: Discussionmentioning
confidence: 96%
“…With a graduate student he embarked on writing numerous proposals to Australian industry to fund the development of a Lotem system. After several smaller grants, he received a larger grant, which allowed him to work with Esso Australia on a survey in Western Australia (Vozoff et al, 1985;Vozoff, 1987, Strack et al, 1989. Subsequently, more work continued in Europe and in Australia mostly in collaboration.…”
Section: Introductionmentioning
confidence: 99%
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“…The transient electromagnetic method belongs to the class of controlled-source electromagnetic geophysical techniques originally used for discrete conductors in base-metal exploration (Wait 1951;Staples 1984). For several decades, it has been applied successfully to hydrocarbon, hydrogeologic, engineering, and geothermal studies (Fitterman and Stewart 1986;Strack et al 1989;McNeill 1990;Nabighian and Macnae 1991;Danielsen et al 2003;Christiansen, Auken and Sørensen 2009;Soupios et al 2009;Spichak and Manzella 2009;Abu Rajab and El-Naqa 2013). More recent improvements in hardware, software, and survey designs have allowed the characterising of geological layers and shallow subsurface mapping (Buselli 1985;Sinha 1990;Danielsen et al 2003; Jørgensen et al 2003;Persson and Erlström 2015;Barsukov and Fainberg 2016).…”
Section: Transient Electromagnetic Methodsmentioning
confidence: 99%
“…Since the vector of response variations, or, lies on the space spanned by U, only the parallel component of the error vector can be explained by Equation (2). Due to the orthogonality of e 1 with respect of all column vectors in U (Uj' j = 1, ... ,N p ), we can say that: 4 and, since e l belongs to the space spanned by U, there exists a set of relative variations of parameters, op, for which,…”
Section: Resolution Conceptsmentioning
confidence: 99%