Zobrazeno 1 - 10
of 27
pro vyhledávání: '"N. C. Ghose"'
Publikováno v:
Geological Journal. 57:5207-5221
Autor:
Abhishek Saha, N. C. Ghose
Publikováno v:
Geological Journal. 54:1927-1949
Publikováno v:
International Kimberlite Conference Extended Abstracts: 1998.
Publikováno v:
Geoscience Frontiers, Vol 8, Iss 4, Pp 809-822 (2017)
The late Aptian (118–115 Ma) continental flood basalts of the Rajmahal Volcanic Province (RVP) are part of the Kerguelen Large Igneous Province, and constitute the uppermost part of the Gondwana Supergroup on the eastern Indian shield margin. The l
Autor:
N. C. Ghose, Nilanjan Chatterjee
Publikováno v:
Gondwana Research. 20:362-379
The Indian Shield was assembled through a Proterozoic collision between the northern and southern Indian continental blocks along the ENE–WSW Central Indian Tectonic Zone (CITZ). Chemical dating of monazite, xenotime and uraninite, and thermobarome
Publikováno v:
Island Arc. 19:336-356
A variety of low- to high-pressure metamorphic assemblages occur in the metabasic rocks and metachert in the Upper Cretaceous–Eocene ophiolite belt of the central part of the Naga Hills, an area in the northern sector of the Indo–Myanmar Ranges i
Autor:
Nilanjan Chatterjee, N. C. Ghose
Publikováno v:
Journal of Metamorphic Geology. 28:209-225
Tectonic slices and lenses of eclogite within mafic and ultramafic rocks of the Early Cretaceous–Eocene Naga Hills ophiolite were studied to constrain the physical conditions of eastward subduction of the Indian plate under the Burma microplate and
Publikováno v:
Precambrian Research. 161:303-316
The thermal-tectonic history of the eastern part of the Chotanagpur gneissic complex (CGC) in the eastern Indian shield was investigated through U–Pb dating of zircon in anorthosite, U–Th–Pb chemical dating of monazite in metapelite granulite,
Autor:
N C Ghose
Publikováno v:
Proceedings of Indian National Science Academy, Vol 39, Iss 3A (2015)
Problem of Alkaline Magma in the Deccan Basalt Province
Publikováno v:
Journal of Asian Earth Sciences. 25:77-94
The Bengal anorthosite occurs as a large tadpole-shaped pluton (250 km 2 ) in the granulite facies terrain of the Proterozoic Chotanagpur Gneiss Granulite Complex at the northeastern edge of the Indian peninsular shield. Its axis of elongation confor