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All the rock magnetic and Paleomagnetic measurements were done atCSIR-NGRI laboratory, Hyderabad, India. At least three specimens per sample were subjected to detailed stepwise alternating field (AF) and/orthermal demagnetization(TD) to a maximum of100 mTor 600 °C in order to separate components based on their coercivity or unblocking temperature.
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Sandra D’Sa, Debasis Patnaik, The Impact of the Pharmaceutical Industry ofHyderabadin the Pollution of the Godavari River, Water Management inSouth Asia, 10.1007/978-3-030-35237-0_3, (23-51), (2020).More Details
Themagnetitefree fractions were further separated using an iso- dynamicmagnetic separatorinto: (1) a pure mafic fraction comprising pyroxene/amphibole (denoted as 'M'); 184 B.K. Pandey et aL/ Precambrian Research 84 (1997) 181 196 Table 1 List of Rb-Sr ages on the rocks of the EDC Area Rock Age (Ma) 87Sr/SaSr Initial Reference Hampi Pink ...More Details
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Paleomagnetism and geochronological studies on a 450 km long 2216 Ma dyke from the Dharwar craton, southernIndia... Dharwar Craton ofsouth Indiais the largest and one of the most extensively studied Archean craton in the Indian Peninsular shield. ...Hyderabad,India(1982), pp. 47-51. Google Scholar.More Details
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