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Artigo de periodico
Mafic dykes at the southwestern margin of Eastern Ghats belt: evidence of rifting and collision (2010)
Bhattacharya, S.; Chaudhary, A. K.; Teixeira, Wilson
Fonte: Journal of Earth System Science. Unidade: IGC
Assuntos: ENXAME DE DIQUES, GEOQUÍMICA, PETROGRAFIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BHATTACHARYA, S. e CHAUDHARY, A. K. e TEIXEIRA, Wilson. Mafic dykes at the southwestern margin of Eastern Ghats belt: evidence of rifting and collision. Journal of Earth System Science, v. 119, n. 6, p. 815-823, 2010Tradução . . Disponível em: https://doi.org/10.1007/s12040-010-0058-x. Acesso em: 08 set. 2024.
APA
Bhattacharya, S., Chaudhary, A. K., & Teixeira, W. (2010). Mafic dykes at the southwestern margin of Eastern Ghats belt: evidence of rifting and collision. Journal of Earth System Science, 119( 6), 815-823. doi:10.1007/s12040-010-0058-x
NLM
Bhattacharya S, Chaudhary AK, Teixeira W. Mafic dykes at the southwestern margin of Eastern Ghats belt: evidence of rifting and collision [Internet]. Journal of Earth System Science. 2010 ; 119( 6): 815-823.[citado 2024 set. 08 ] Available from: https://doi.org/10.1007/s12040-010-0058-x
Vancouver
Bhattacharya S, Chaudhary AK, Teixeira W. Mafic dykes at the southwestern margin of Eastern Ghats belt: evidence of rifting and collision [Internet]. Journal of Earth System Science. 2010 ; 119( 6): 815-823.[citado 2024 set. 08 ] Available from: https://doi.org/10.1007/s12040-010-0058-x
Artigo de periodico
Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm-Nd isotopic evidence (2004)
Bhattacharya, S.; Swain, A. K.; Teixeira, Wilson
Fonte: Gondwana research. Unidade: IGC
Assuntos: ISÓTOPOS, ÍNDIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BHATTACHARYA, S. e SWAIN, A. K. e TEIXEIRA, Wilson. Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm-Nd isotopic evidence. Gondwana research, v. 7, n. 2, p. 627-629, 2004Tradução . . Disponível em: https://doi.org/10.1016/S1342-937X(05)70814-5. Acesso em: 08 set. 2024.
APA
Bhattacharya, S., Swain, A. K., & Teixeira, W. (2004). Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm-Nd isotopic evidence. Gondwana research, 7( 2), 627-629. doi:10.1016/S1342-937X(05)70814-5
NLM
Bhattacharya S, Swain AK, Teixeira W. Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm-Nd isotopic evidence [Internet]. Gondwana research. 2004 ; 7( 2): 627-629.[citado 2024 set. 08 ] Available from: https://doi.org/10.1016/S1342-937X(05)70814-5
Vancouver
Bhattacharya S, Swain AK, Teixeira W. Crustal source for a syenite complex in the high-grade Eastern Ghats belt, India: Sm-Nd isotopic evidence [Internet]. Gondwana research. 2004 ; 7( 2): 627-629.[citado 2024 set. 08 ] Available from: https://doi.org/10.1016/S1342-937X(05)70814-5
Artigo de periodico
High-temperature crustal anatexis in a clockwise P-T-t path: isotopic evidence from a granulite-granitoid suite in the Eastern Ghats belt, India (2003)
Bhattacharya, S.; Kar, Rajib; Teixeira, Wilson ; Basei, Miguel Angelo Stipp
Fonte: Journal of the Geological Society. Unidade: IGC
Assuntos: ISÓTOPOS, OROGÊNESE, ÍNDIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
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: 08 set. 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:10.1144/0016-764902-063
NLM
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 set. 08 ] Available from: https://doi.org/10.1144/0016-764902-063
Vancouver
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 set. 08 ] Available from: https://doi.org/10.1144/0016-764902-063
Artigo de periodico
Grenvillian thermal event and remnant charnockite: isotopic evidence from the Chilka lake granulite-migmatite suite in the eastern Ghasts belt, India (2002)
Bhattacharya, S.; Deomurari, M. P.; Teixeira, Wilson
Fonte: Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences. Unidade: IGC
Assunto: GEOCRONOLOGIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BHATTACHARYA, S. e DEOMURARI, M. P. e TEIXEIRA, Wilson. Grenvillian thermal event and remnant charnockite: isotopic evidence from the Chilka lake granulite-migmatite suite in the eastern Ghasts belt, India. Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences, v. 111, n. 4, p. 391-399, 2002Tradução . . Disponível em: https://doi.org/10.1007/bf02702052. Acesso em: 08 set. 2024.
APA
Bhattacharya, S., Deomurari, M. P., & Teixeira, W. (2002). Grenvillian thermal event and remnant charnockite: isotopic evidence from the Chilka lake granulite-migmatite suite in the eastern Ghasts belt, India. Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences, 111( 4), 391-399. doi:10.1007/bf02702052
NLM
Bhattacharya S, Deomurari MP, Teixeira W. Grenvillian thermal event and remnant charnockite: isotopic evidence from the Chilka lake granulite-migmatite suite in the eastern Ghasts belt, India [Internet]. Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences. 2002 ; 111( 4): 391-399.[citado 2024 set. 08 ] Available from: https://doi.org/10.1007/bf02702052
Vancouver
Bhattacharya S, Deomurari MP, Teixeira W. Grenvillian thermal event and remnant charnockite: isotopic evidence from the Chilka lake granulite-migmatite suite in the eastern Ghasts belt, India [Internet]. Proceedings of the Indian Academy of Sciences. Earth and Planetary Sciences. 2002 ; 111( 4): 391-399.[citado 2024 set. 08 ] Available from: https://doi.org/10.1007/bf02702052
Artigo de periodico
Early archaean continental crust in the eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite (2001)
Bhattacharya, S.; Kar, Rajib; Misra, S.; Teixeira, Wilson
Fonte: Geological Magazine. Unidade: IGC
Assuntos: GEOCRONOLOGIA, PETROLOGIA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BHATTACHARYA, S. et al. Early archaean continental crust in the eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite. Geological Magazine, v. 138, n. 5, p. 609-618, 2001Tradução . . Disponível em: https://doi.org/10.1017/s0016756801005702. Acesso em: 08 set. 2024.
APA
Bhattacharya, S., Kar, R., Misra, S., & Teixeira, W. (2001). Early archaean continental crust in the eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite. Geological Magazine, 138( 5), 609-618. doi:10.1017/s0016756801005702
NLM
Bhattacharya S, Kar R, Misra S, Teixeira W. Early archaean continental crust in the eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite [Internet]. Geological Magazine. 2001 ; 138( 5): 609-618.[citado 2024 set. 08 ] Available from: https://doi.org/10.1017/s0016756801005702
Vancouver
Bhattacharya S, Kar R, Misra S, Teixeira W. Early archaean continental crust in the eastern Ghats granulite belt, India: isotopic evidence from a charnockite suite [Internet]. Geological Magazine. 2001 ; 138( 5): 609-618.[citado 2024 set. 08 ] Available from: https://doi.org/10.1017/s0016756801005702

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