The mineralogical status of ilmenite from a prominent modern placer de
posit of India is illustrated using different techniques. Compositiona
l, powder XRD, TGA and SEM analyses prove that consistent low temperat
ure alteration took place in Chavara ilmenite leading to the formation
of a pseudorutile-hydrated-ilmenite stage. Except for the indication
of a geochemical zonation at the southern tip of the deposit, the Chav
ara ilmenite points to a common origin throughout its 22 km stretch al
ong the coast. We advocate a major segregation activity by marine fact
ors to the accumulated sediments in the shelf zone in order to origina
te such a huge deposit of homogeneous composition.