Add to ORKGA single deep-sea core (MD982156) of 30.30 meters long which is obtained during the MD III-IMAGES IV Expedition from Roo Rise - Indian Ocean in 1998 was studied. Down to 30 meters of the core length, the sediment consists of abundance planktonic foraminiferas. Below 30 meters, it is mostly composed of phillipsite mineral-rich sediment that is associated with nannoplanktons.The Paleocene authigenic phillipsite minerals associated with nannoplanktons is separated from Late Miocene to Holocene planktonic foraminiferas rich-sediments by hiatus. This hiatus or non deposi- tional in Roo Rise suggest be triggered by long Cenozoic tectonic erosion
Of the eight piston cores from the deep-sea floor of the Indian Ocean, two contained abundant plankt...
Of the several sites drilled during Leg 22, Site 214 is of special interest to biostratigraphers bec...
The Osborn Plateau is a large intraplate elevation in the eastern Indian Ocean, which has been poorl...
A single deep-sea core (MD982156) of 30.30 meters long which is obtained during the MD III-IMAGES IV...
During the MD III - IMAGES IV Expedition, one of the cores that has length around 30.30 m below sea ...
DOI: 10.17014/ijog.v5i1.92The sample studied was derived from the base of core MD 982156, one of the...
Deep-sea cores recovered from the N.W. Indian Ocean during Leg 23 of the Deep-Sea Drilling Project w...
Present study is the phillipsite grains present in a siliceous sediment core (water depth 5100 m) re...
1121-1131Present study is the phillipsite grains present in a siliceous sediment core (water depth 5...
A pulse of intense carbonate dissolution occurred during the early late Paleocene at 58.4 Ma. A prom...
A significant and abrupt change in the sedimentary regime at Site 237 provides evidence for an early...
Correlation of mineral associations from sediment recovered on the northwestern Australian continent...
18-34Deep Sea Drilling Project Site 219 on the Laccadive Ridge penetrates Pleistocene to upper Paleo...
A major change in Cenozoic deep-sea benthic foraminifera occurred in the Atlantic, Indian, and Pacif...
Phosphorites were dredged from the flanks of the Error Seamount, off the Somali coast from depths of...
Of the eight piston cores from the deep-sea floor of the Indian Ocean, two contained abundant plankt...
Of the several sites drilled during Leg 22, Site 214 is of special interest to biostratigraphers bec...
The Osborn Plateau is a large intraplate elevation in the eastern Indian Ocean, which has been poorl...
A single deep-sea core (MD982156) of 30.30 meters long which is obtained during the MD III-IMAGES IV...
During the MD III - IMAGES IV Expedition, one of the cores that has length around 30.30 m below sea ...
DOI: 10.17014/ijog.v5i1.92The sample studied was derived from the base of core MD 982156, one of the...
Deep-sea cores recovered from the N.W. Indian Ocean during Leg 23 of the Deep-Sea Drilling Project w...
Present study is the phillipsite grains present in a siliceous sediment core (water depth 5100 m) re...
1121-1131Present study is the phillipsite grains present in a siliceous sediment core (water depth 5...
A pulse of intense carbonate dissolution occurred during the early late Paleocene at 58.4 Ma. A prom...
A significant and abrupt change in the sedimentary regime at Site 237 provides evidence for an early...
Correlation of mineral associations from sediment recovered on the northwestern Australian continent...
18-34Deep Sea Drilling Project Site 219 on the Laccadive Ridge penetrates Pleistocene to upper Paleo...
A major change in Cenozoic deep-sea benthic foraminifera occurred in the Atlantic, Indian, and Pacif...
Phosphorites were dredged from the flanks of the Error Seamount, off the Somali coast from depths of...
Of the eight piston cores from the deep-sea floor of the Indian Ocean, two contained abundant plankt...
Of the several sites drilled during Leg 22, Site 214 is of special interest to biostratigraphers bec...
The Osborn Plateau is a large intraplate elevation in the eastern Indian Ocean, which has been poorl...