2006
DOI: 10.1016/j.gr.2005.11.014
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Analysis of airborne magnetic and gravity anomalies of peninsular shield, India integrated with seismic and magnetotelluric results and gravity anomalies of Madagascar, Sri Lanka and East Antarctica

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Cited by 25 publications
(25 citation statements)
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“…In these models, moderate low resistivity zones are confined to the region near the PCSZ. Also, a remodeling of gravity data (Mishra et al, 2006) yielded a model involving three layered crust with 2.7, 2.8 and 2.9 gm/cm 3 with thicknesses around 12, 13 and 17 km, respectively without any low density layer (of 2.65 gm/cm 3 ) in the mid-crust (Fig. 5).…”
Section: Discussionmentioning
confidence: 99%
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“…In these models, moderate low resistivity zones are confined to the region near the PCSZ. Also, a remodeling of gravity data (Mishra et al, 2006) yielded a model involving three layered crust with 2.7, 2.8 and 2.9 gm/cm 3 with thicknesses around 12, 13 and 17 km, respectively without any low density layer (of 2.65 gm/cm 3 ) in the mid-crust (Fig. 5).…”
Section: Discussionmentioning
confidence: 99%
“…Another study identified a denser lower crust (2.85 gm/cm 3 ) with Moho depth ranging from 36 to 41 km (Ajayakumar et al, 2006). Excluding the earlier model by Singh et al (2003), all the other models (Radhakrishna et al, 2003;Ajayakumar et al, 2006;Mishra et al, 2006; show that the density of mid-lower crustal layers is more than about 2.75 gm/cm 3 for PCSZ and adjoining areas, suggesting relatively high density material beneath this zone.…”
Section: Gravity Studiesmentioning
confidence: 91%
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