Mohanti M., Srivastava S. C. Oligocene reefal environment of Kutch Basin (Western India) with implications of the Mediterranean connection. In: Géologie Méditerranéenne. Tome 21, numéro 3-4, 1994. Perimediterranean carbonate platforms. First International Meeting. Marseille – France (5-8 septembre 1994) sous la direction de Jean-Pierre Masse. pp. 127-129
International audienceThe Western Indian Ocean results from a complex geological history, implying b...
Eustacy was the dominant factor influencing the Gulf of Martaban Field isolated platform, subdivided...
International audienceIsolated carbonate platforms occur throughout the geologic record, from Archea...
Mohanti M., Srivastava S. C. Oligocene reefal environment of Kutch Basin (Western India) with implic...
Middle Eocene Fulra Limestone and Oligocene Maniyara Fort Formation represent platform carbonate dep...
Due to its intermediate geographical position between the Mediterranean and W Pacific, the Oligocen...
Major, trace, and rare-earth element (REE) analyses of larger benthic foraminifera-bearing carbonate...
The late Oligocene-early Miocene mixed carbonate-siliciclastic deposits of Kutch developed on the st...
The Kutch Basin is unique among the western Indian sedimentary basins because of its near‐complete s...
Due to its intermediate geographical position between the Mediterranean and W Pacific, the Oligocene...
Stable isotope analyses have been carried out on rocks and fossils of the Palaeogene carbonate-clast...
The Paleogene sections of Kutch are the reference for the regional chronostratigraphic units of Indi...
A combined micropalaeontological and sedimentological investigation of the Early Eocene Naredi Forma...
International audienceThe Western Indian Ocean results from a complex geological history, implying b...
Eustacy was the dominant factor influencing the Gulf of Martaban Field isolated platform, subdivided...
International audienceIsolated carbonate platforms occur throughout the geologic record, from Archea...
Mohanti M., Srivastava S. C. Oligocene reefal environment of Kutch Basin (Western India) with implic...
Middle Eocene Fulra Limestone and Oligocene Maniyara Fort Formation represent platform carbonate dep...
Due to its intermediate geographical position between the Mediterranean and W Pacific, the Oligocen...
Major, trace, and rare-earth element (REE) analyses of larger benthic foraminifera-bearing carbonate...
The late Oligocene-early Miocene mixed carbonate-siliciclastic deposits of Kutch developed on the st...
The Kutch Basin is unique among the western Indian sedimentary basins because of its near‐complete s...
Due to its intermediate geographical position between the Mediterranean and W Pacific, the Oligocene...
Stable isotope analyses have been carried out on rocks and fossils of the Palaeogene carbonate-clast...
The Paleogene sections of Kutch are the reference for the regional chronostratigraphic units of Indi...
A combined micropalaeontological and sedimentological investigation of the Early Eocene Naredi Forma...
International audienceThe Western Indian Ocean results from a complex geological history, implying b...
Eustacy was the dominant factor influencing the Gulf of Martaban Field isolated platform, subdivided...
International audienceIsolated carbonate platforms occur throughout the geologic record, from Archea...