1983
DOI: 10.1190/1.1441522
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Three‐dimensional model of the Koyna area of Maharashtra State (India) based on the spectral analysis of aeromagnetic data

Abstract: The estimation of thickness of trap rocks in the earthquake‐affected Koyna area is an important parameter for revealing the topography that existed before the Deccan volcanism. In the present work, a case history is presented delineating a three‐dimensional block model for the Koyna area by the spectral analysis of aeromagnetic data. The thickness in the area was found to vary from 700 to 2200 m, which correlates well with the results of other geophysical investigations.

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Cited by 39 publications
(24 citation statements)
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“…These results clearly show that the epicentral zone is characterised by higher velocities in the crustal part. It is interesting to examine the aeromagnetic data acquired in the Koyna region over 13 short profiles each of 100 km in length at spacing of 4 km [Negi et al, 1983]. The seismic zone is also mapped as magnetic lineament from aeromagnetic studies [Talwani, 1997] In KSZ the seismicity is associated with the high velocity anomaly and this feature could be associated with more brittle and competent rock with ability to store strain energy and release it as brittle failure.…”
Section: Discussionmentioning
confidence: 99%
“…These results clearly show that the epicentral zone is characterised by higher velocities in the crustal part. It is interesting to examine the aeromagnetic data acquired in the Koyna region over 13 short profiles each of 100 km in length at spacing of 4 km [Negi et al, 1983]. The seismic zone is also mapped as magnetic lineament from aeromagnetic studies [Talwani, 1997] In KSZ the seismicity is associated with the high velocity anomaly and this feature could be associated with more brittle and competent rock with ability to store strain energy and release it as brittle failure.…”
Section: Discussionmentioning
confidence: 99%
“…The lateral extent of this fault is between the Koyna Dam and the right angle turn to the east in the Koyna River. Both the aeromagnetic data (NEGI et al, 1983) and seismic refraction data (KAILA et al, 1981) show that on a E-W profile through Koyna, the basalt is thicker under Koyna than under Alore to its west. The aeromagnetic data also show that there is a N -S to N10°E-S10°W trending fault along the Koyna River that extends at least 40 km to the south.…”
Section: B Koyna-ri6er Fault Zonementioning
confidence: 99%
“…In an effort to determine the thickness of the Deccan Trap rocks in the Koyna area, aeromagnetic data were acquired on 13 short profiles, each about 100 km long and spaced at 4 km (NEGI et al, 1983). Data were recorded at elevations of 1220, 1524 and 2134 m, above mean sea level.…”
Section: D3 Aeromagnetic Datamentioning
confidence: 99%
“…The utility of the Fourier spectral technique has been well established in estimating the average depth to various subsurface discontinuities from the potential field data (Spector and Grant 1970;Hahn et al 1976;Negi et al 1983Negi et al , 1986aNegi and Agrawal 1986). This technique treats the observed potential field anomalies, originating from line sources at various subsurface levels, as a statistical population.…”
Section: Spectral Analysismentioning
confidence: 99%