R. Shankar et al., MAGNETIC-SUSCEPTIBILITY STUDIES OF SURFICIAL SEDIMENTS FROM THE DEEP ARABIAN SEA, Journal of the Geological Society of India, 43(2), 1994, pp. 159-167
A wide variety of processes such as volcanic activity, submarine and c
ontinental weathering, aeolian transport and authigenesis can account
for the magnetic susceptibility of the deep Arabian Sea sediments. Pre
liminary studies of the magnetic fraction indicate that it is predomin
antly composed of pseudo-single domain and viscous magnetite. It is fo
und that magnetic susceptibility can be used to estimate the approxima
te iron content of marine sediments.