Sedimentation regimes are an important control on the distribution of
marine mineral resources worldwide. In the eastern Indian Ocean, phosp
horites are associated with organic-rich sediments including coral ree
fs on continental margin areas, principally off western India, and pos
sibly occur on seamounts throughout the equatorial and subequatorial p
arts of the region. Metalliferous sediments and polymetallic sulfides
can be expected to be located in areas of volcaniclastic and hydrother
mal sedimentation in and near the Indonesian Island arcs and on the mi
d-ocean ridge system, the Southeast Indian Ridge. Manganese nodules ar
e both abundant and high grade in the central Indian Basin in associat
ion with slowly accumulating manganese-rich pelagic clays, and sedimen
t data suggest that a similar situation may prevail in the Wharton Bas
in.