DRS at CSIR-National Institute of Oceanography
- » sup(234) Th scavenging and particle export fluxes from the upper 100 m of the Arabian Sea
- » Seasonal changes of the sediment size distribution and stability along the beaches of...
- » Potential distribution of subsurface methane in the sediments of the eastern Arabian...
- » Growing need to study foraminifera in the laboratory culture experiments: An attempt...
- » Acoustic basement: Its relevance to Karwar port development
- » Foraminiferal fauna from the Cochin backwaters: Biological indicators of man-made...
- » Impact microcraters on an Australasian microtektite
- » Record of the Cretaceous magnetic quiet zone in the distal Bengal fan and its...
- » Potentiality of foraminifera in deciphering paleo-sea levels
- » Onset of an arid climate at 3.5 ka in the tropics: Evidence from monsoon upwelling record
- » Gas-charged sediments in shallow waters off Redi along the central west coast of India
- » 1300 km long late Pleistocene-Holocene shelf edge barrier reef system along the western...
- » The fate of sand dunes of Goa
- » Geotechnical properties of marine soil off north Konkan Coast
- » Heavy mineral distribution in the surficial sediments from the eastern continental...
- » Signatures of rare-earth elements in banded corals of Kalpeni atoll-Lakshadweep...
- » Genesis of apatite in the phosphatized limestones of the western continental shelf of...
- » Quantitative radiolarian assemblages in surface sediments from the central Indian Basin...
- » Evidence for hydrothermal activity in the Andaman Backarc Basin
- » Trade routes and communication pattern of ancient Orissa
- » Marine archaeological aspects
- » Effect of exposure angle on the marine atmospheric corrosion of mild steel
- » Some observations on use of siliceous mineral waters in reduction of corrosion in RCC...
- » Effect of exposure angle on the marine atmospheric corrosion of mild steel
- » Some observations on use of siliceous mineral waters in reduction of corrosion in RCC...