Bhattacharya, S.; Kar, Rajib; Teixeira, Wilson 
; Basei, Miguel Angelo Stipp
Source: Journal of the Geological Society. Unidade: IGC
Subjects: ISÓTOPOS, OROGÊNESE, ÍNDIA
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ABNT
BHATTACHARYA, S. et al. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India. Journal of the Geological Society, v. 160, n. 1, p. 39-46, 2003Tradução . . Disponível em: https://doi.org/10.1144/0016-764902-063. Acesso em: 27 jul. 2024.APA
Bhattacharya, S., Kar, R., Teixeira, W., & Basei, M. A. S. (2003). High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India. Journal of the Geological Society, 160( 1), 39-46. doi:10.1144/0016-764902-063NLM
Bhattacharya S, Kar R, Teixeira W, Basei MAS. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India [Internet]. Journal of the Geological Society. 2003 ; 160( 1): 39-46.[citado 2024 jul. 27 ] Available from: https://doi.org/10.1144/0016-764902-063Vancouver
Bhattacharya S, Kar R, Teixeira W, Basei MAS. High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India [Internet]. Journal of the Geological Society. 2003 ; 160( 1): 39-46.[citado 2024 jul. 27 ] Available from: https://doi.org/10.1144/0016-764902-063
