2011
DOI: 10.5194/npg-18-179-2011
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Inversion of Schlumberger resistivity sounding data from the critically dynamic Koyna region using the Hybrid Monte Carlo-based neural network approach

Abstract: Abstract. Koyna region is well-known for its triggered seismic activities since the hazardous earthquake of M = 6.3 occurred around the Koyna reservoir on 10 December 1967. Understanding the shallow distribution of resistivity pattern in such a seismically critical area is vital for mapping faults, fractures and lineaments. However, deducing true resistivity distribution from the apparent resistivity data lacks precise information due to intrinsic non-linearity in the data structures. Here we present a new tec… Show more

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Cited by 42 publications
(28 citation statements)
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References 51 publications
(53 reference statements)
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“…This method provides the apparent resistivity distribution against depth. The depth of penetration of electrical signal is generally found to be approximately one-third of the distance between the electrode separations (Dahlin 2000;Maiti et al 2011). This method is carried out to decipher problems of aquifer in hard formation such as the Deccan Trap region.…”
Section: Survey Designmentioning
confidence: 98%
“…This method provides the apparent resistivity distribution against depth. The depth of penetration of electrical signal is generally found to be approximately one-third of the distance between the electrode separations (Dahlin 2000;Maiti et al 2011). This method is carried out to decipher problems of aquifer in hard formation such as the Deccan Trap region.…”
Section: Survey Designmentioning
confidence: 98%
“…In view of the established utility of resistivity method in locating and demarcating the fractured and weathered zones especially in the Tenduli-Vengurla, Konkan region, it was worth to conduct electrical resistivity experiment over the area. The Direct Current (DC) resistivity sounding method has extensively been used for solving hydrological, geothermal, environmental and engineering problems (Zohdy, 1989;Gupta et al, 2010b;Maiti et al, 2011). The method provides the apparent resistivity distribution against depth.…”
Section: Introductionmentioning
confidence: 99%
“…These schemes have been widely applied to solve non-linear problems in almost all branches of geophysics (e.g., Van der Bann and Jutten, 2000;Poulton, 2001). For example: (1) for seismic event classification (Dystart and Pulli, 1990), (2) well log analysis (Aristodemou et al, 2005;Maiti et al, 2007;Tiwari, 2009, 2010b), (3) first arrival picking (Murat and Rudman, 1993), (4) earthquake time series modeling (Feng et al, 1997), (5) inversion (Raiche, 1991;Devilee et al, 1999), (6) parameter estimation in geophysics (Macias et al, 2000), (7) prediction of aquifer water level (Coppola et al, 2005;Tsanis et al, 2008), (8) magneto-telluric data inversion (Spichak and Popova, 2000), (9) magnetic interpretations (Bescoby et al, 2006), (10) signal discrimination (Maiti and Tiwari, 2010a), (11) DC resistivity inversion (Qady and Ushijima, 2001;Singh et al, 2010;Maiti et al, 2011). There are, however, several limitations in conventional neural network approaches (Bishop, 1995;Maiti and Tiwari, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…The MCMC inversion technique has previously been applied for geo-electromagnetic data in relatively simple 1D models with satisfactory results, for example, magnetotelluric (MT; Grandis et al 1999;Guo et al 2011), DC resistivity (Schott et al 1999;Maiti et al 2011), and Controlled-Source Audio-frequency MT (CSAMT; Grandis and Sumintadiredja 2013) studies. Despite the simplicity of the 1D models in geoelectromagnetics, their inversions involve highly nonlinear problems demanding non-linear or global search approaches to avoid fundamental limitations of the linearized approach (Sen and Stoffa 1996;Sambridge and Mosegaard 2002).…”
Section: Introductionmentioning
confidence: 99%