Palaeomagnetic and rock magnetic studies on the dykes of Goa, west coast of Indian Precambrian Shield

Detailed alternating field (AF) and thermal demagnetization techniques on 120 samples belonging to 10 dykes of the Goa region along the west coast of the Indian Precambrian Shield, have yielded characteristic remanent magnetization (ChRM) directions from 9 dykes of which 6 dykes exhibited a reverse magnetic polarity direction (D = 150degrees, 1 = 44.30degrees, k := 58, alpha(95) = 5.8, N = 6 dykes), while 3 dykes exhibited normal polarity D = 351degrees, 1 = -50degrees, k = 21, alpha(95) = 14.9, N = 3 dykes) direction. The remaining I dyke has shown stable direction, but with a strong overprint of the present earth field (PEF) direction, which could not be removed by either AF or thermal cleaning techniques. A Palaeomagnetic pole, computed by averaging the VGPs of 9 dykes is situated at 41.2degreesN 78.1degreesW (N = 9 dykes; A(95) = 9.81degrees), which is close to that of the Deccan super pole (36.9degreesN, 78.8degreesW), suggesting that the dykes in the Goa region are related to the Deccan basaltic eruptions. Recently published 40Ar/39Ar dating on the normal polarity dykes of the studied area have assigned the ages as 62.8 +/- 0.2 Ma. These results demonstrate that the Deccan magnetism continued to affect western India for at least 1-2 Ma after the peak Deccan eruption during the K-T boundary. On the basis of published geological and geochernical information along with our Palaeomagnetic results, these intrusive bodies could be attributed as the feeders for the uppermost fort-nations of Wai subgroup of the Western Ghat Deccan basalts, or to the major geodynamic events such as the opening of the Arabian Sea and the rifting of the Seychelles-Mascarene oceanic plateau, which occurred soon after the cessation of the Deccan volcanism. Rock magnetic experiments such as the Lowrie-Fuller test along with low-temperature magnetic susceptibility and isothermal remanent magnetization (IRM) measurements have identified single domain (SD) type titano-magnetite as the major characteristic remanent magnetization carrying magnetic mineral in the dyke samples. (C) 2002 Published by Elsevier Science B.V.