Zobrazeno 1 - 10
of 24
pro vyhledávání: '"P. V. Sunder Raju"'
Publikováno v:
Journal of the Geological Society of India. 98:1217-1220
Publikováno v:
Journal of the Geological Society of India. 98:181-184
Publikováno v:
Journal of Earth System Science. 131
Publikováno v:
Geologica Acta, Vol 13, Iss 4 (2015)
The Mesoarchean chromitites in the Singhbhum craton provide the main source of chromium in India. We report here results of dating zircon grains that were found in the chromitite of ultramafic rocks belonging to the southern part of the Archean Baula
Externí odkaz:
https://doaj.org/article/03383f89c2ec469e947b93d6d0f8cc00
Autor:
P. V. Sunder Raju
Publikováno v:
Journal of the Geological Society of India. 96:250-252
The REE-2 is a carbonatite sample with rare earth elements provided from a Canadian mining company and distributed by Canadian Certified Reference Materials (CCRM), Canada. The reference material was provided to participate in the testing process (ro
Autor:
P. V. Sunder Raju
Publikováno v:
Journal of the Geological Society of India. 94:47-52
This study was carried out on chromitite bearing samples from Sittampundi anorthosite complex (SAC), Tamil Nadu, to understand the morphology of platinum-group minerals (PGM) and associated silicates using state-of-the-art technology QEMSCAN®. The d
Publikováno v:
Earth-Science Reviews. 188:427-440
India has perhaps the richest Paleoarchean to Paleoproterozoic crustal components on Earth ( Miller et al., 2018 ). Notwithstanding this, much of the Indian subcontinent remains unexplored compared to other ancient cratons in North America, Australia
Publikováno v:
Annals of Phytomedicine: An International Journal. 9
Autor:
P V SUNDER RAJU
Publikováno v:
Goldschmidt Abstracts.
Autor:
P. V. Sunder Raju, Rajat Mazumder
Publikováno v:
Earth-Science Reviews. 202:102999
The Dharwar Craton is the largest Archean cratonic nuclei of India and is made up of western and eastern blocks separated by the 2.5 Ga Closepet granite batholith. The Western Dharwar Craton consists mostly of 3.3–3.0 Ga TTG (the Peninsular Gneissi