Articles written in Journal of Earth System Science
Volume 114 Issue 5 October 2005 pp 505-514
The Deccan Volcanic Province (DVP) of India, as a whole, faces a severe shortage of water despite receiving a high annual rainfall, this is primarily due to excess runoff and lack of water conservation practices. In this study, an attempt is made to identify zones favourable for the application and adaptation of site-specific artificial-recharge techniques for augmentation of groundwater through a Geographical Information System (GIS) based hydrogeomorphic approach in the Bhatsa and Kalu river basins of Thane district, in western DVP. The criteria adopted for the GIS analysis were based on the hydrogeomorphological characteristics of both basins extracted from the IRS-1C LISS-III data supported by information on drainage pattern, DEM derived slope, lineament density, drainage density, and groundwater condition. The integrated study helps design a suitable groundwater management plan for a basaltic terrain.
Volume 127 Issue 1 February 2018 Article ID 0003
Here we report new paleomagnetic results and precise paleopole position of the extensional study on ~ 2367 Ma mafic giant radiating dyke swarm in the Dharwar craton, southern India. We have sampled 29 sites on 12 dykes from NE–SW Karimnagar–Hyderabad dykes and Dhone–Gooty sector dykes, eastern Dharwar craton to provide unambiguous paleomagnetism evidence on the spectacular radiating dyke swarm and thereby strengthening the presence of single magmatic event at ~ 2367 Ma. A total of 158 samples were subjected to detailed alternating field and thermal demagnetization techniques and the results are presented here along with previously reported data on the same dyke swarm. The remanent magnetic directions are showing two components, viz., seven sites representing four dykes show component (A) with mean declination of 94◦ and mean inclination of −70◦ (k = 87, α95 = 10◦) and corresponding paleopole at 16◦N, 41◦E (dp = 15◦ and dm = 17◦) and 22 sites representing 8 dykes yielded a component (B) with mean declination of 41◦ and mean inclination of −21◦ (k = 41, α95 = 9◦) with a paleopole at 41◦N, 200◦E (dp = 5◦ and dm = 10◦). Component (A) results are similar to the previously reported directions from the ~ 2367 Ma dyke swarm, which have been confirmed fairly reliably to be of primary origin. The component (B) directions appear to be strongly overprinted by the 2080 Ma event. The grand mean for the primary component (A) combined with earlier reported studies gives mean declination of 97◦ and mean inclination of −79◦ (k = 55, α95 = 3◦) with a paleopole at 15◦N, 57◦E (dp = 5◦, dm = 6◦). Paleogeographical position for the Dharwar craton at ~ 2367 Ma suggests that there may be a chance to possible spatial link between Dharwar dykes of Dharwar craton (India), Widgemooltha and Erayinia dykes of Yilgarn craton (Australia), Sebanga Poort Dykes of Zimbabwe craton (Africa) and Karelian dykes of Kola-Karelia craton (Baltica Shield).
Volume 128 | Issue 8
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