DRS at National Institute Of Oceanography >
Institute's contributions >
Microtexture and distribution of minerals in hydrothermal Barite-Silica chimney from the Franklin seamount, SW Pacific: Constraints on mode of formation.
Revisiting the structure, age, and evolution of the Wharton Basin to better understand subduction under Indonesia.
Cyclicity in the Late Holocene monsoonal changes from the western Bay of Bengal: Foraminiferal approach.
Post-monsoon equilibrium beach profiles and longshore sediment transport rates at Candolim, Miramar and Keri beaches of Goa, India.
Refractory metal nuggets in different types of cosmic spherules.
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