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Artigo de periodico
LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile (2015)
Hyppolito, Thais Nogueira; Juliani, Caetano ; García-Casco, Antonio ; Meira, Vinícius Tieppo ; Bustamante, Andrés ; Hall, C.
Source: Journal of Metamorphic Geology. Unidades: IGC, IAG
Subjects: METAMORFISMO, PALEOZOICO
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
HYPPOLITO, Thais Nogueira et al. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile. Journal of Metamorphic Geology, v. 33, n. 9, p. 1003-1024, 2015Tradução . . Disponível em: https://doi.org/10.1111/jmg.12166. Acesso em: 05 out. 2024.
APA
Hyppolito, T. N., Juliani, C., García-Casco, A., Meira, V. T., Bustamante, A., & Hall, C. (2015). LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile. Journal of Metamorphic Geology, 33( 9), 1003-1024. doi:10.1111/jmg.12166
NLM
Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante A, Hall C. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile [Internet]. Journal of Metamorphic Geology. 2015 ; 33( 9): 1003-1024.[citado 2024 out. 05 ] Available from: https://doi.org/10.1111/jmg.12166
Vancouver
Hyppolito TN, Juliani C, García-Casco A, Meira VT, Bustamante A, Hall C. LP/HT metamorphism as a temporal marker of change of deformation style within the Late Palaeozoic accretionary wedge of central Chile [Internet]. Journal of Metamorphic Geology. 2015 ; 33( 9): 1003-1024.[citado 2024 out. 05 ] Available from: https://doi.org/10.1111/jmg.12166
Parte de monografia/livro
New Evidence for Putumayo Crust in the Basement of the Falcon Basin and Guajira Peninsula, Northwestern Venezuela (2015)
Baquero, Marvin; Grande, Sebastian; Urbani, Franco ; Cordani, Umberto G. ; Hall, Chris; Armstrong, Richard
Source: Petroleum Geology and Potential of the Colombian Caribbean Margin, Memoir 108. Unidade: IGC
Subjects: GEOCRONOLOGIA, NEOTECTÔNICA, METAMORFISMO
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BAQUERO, Marvin et al. New Evidence for Putumayo Crust in the Basement of the Falcon Basin and Guajira Peninsula, Northwestern Venezuela. Petroleum Geology and Potential of the Colombian Caribbean Margin, Memoir 108. Tradução . Tulsa: AAPG, 2015. p. 103-136. Disponível em: https://doi.org/10.1306/13531933m1083639. Acesso em: 05 out. 2024.
APA
Baquero, M., Grande, S., Urbani, F., Cordani, U. G., Hall, C., & Armstrong, R. (2015). New Evidence for Putumayo Crust in the Basement of the Falcon Basin and Guajira Peninsula, Northwestern Venezuela. In Petroleum Geology and Potential of the Colombian Caribbean Margin, Memoir 108 (p. 103-136). Tulsa: AAPG. doi:10.1306/13531933m1083639
NLM
Baquero M, Grande S, Urbani F, Cordani UG, Hall C, Armstrong R. New Evidence for Putumayo Crust in the Basement of the Falcon Basin and Guajira Peninsula, Northwestern Venezuela [Internet]. In: Petroleum Geology and Potential of the Colombian Caribbean Margin, Memoir 108. Tulsa: AAPG; 2015. p. 103-136.[citado 2024 out. 05 ] Available from: https://doi.org/10.1306/13531933m1083639
Vancouver
Baquero M, Grande S, Urbani F, Cordani UG, Hall C, Armstrong R. New Evidence for Putumayo Crust in the Basement of the Falcon Basin and Guajira Peninsula, Northwestern Venezuela [Internet]. In: Petroleum Geology and Potential of the Colombian Caribbean Margin, Memoir 108. Tulsa: AAPG; 2015. p. 103-136.[citado 2024 out. 05 ] Available from: https://doi.org/10.1306/13531933m1083639
Artigo de periodico
Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S) (2014)
Hyppolito, Thais Nogueira; García-Casco, Antonio ; Juliani, Caetano ; Meira, Vinícius Tieppo ; Hall, C.
Source: Lithos. Unidade: IGC
Subjects: METAMORFISMO, GONDWANA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
HYPPOLITO, Thais Nogueira et al. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S). Lithos, v. 206-207, p. 409-434, 2014Tradução . . Disponível em: https://doi.org/10.1016/j.lithos.2014.07.023. Acesso em: 05 out. 2024.
APA
Hyppolito, T. N., García-Casco, A., Juliani, C., Meira, V. T., & Hall, C. (2014). Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S). Lithos, 206-207, 409-434. doi:10.1016/j.lithos.2014.07.023
NLM
Hyppolito TN, García-Casco A, Juliani C, Meira VT, Hall C. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S) [Internet]. Lithos. 2014 ; 206-207 409-434.[citado 2024 out. 05 ] Available from: https://doi.org/10.1016/j.lithos.2014.07.023
Vancouver
Hyppolito TN, García-Casco A, Juliani C, Meira VT, Hall C. Late Paleozoic onset of subduction and exhumation at the western margin of Gondwana (Chilenia Terrane): counterclockwise P–T paths and timing of metamorphism of deep-seated garnet–mica schist and amphibolite of Punta Sirena, Coastal Accretionary Complex, central Chile (34° S) [Internet]. Lithos. 2014 ; 206-207 409-434.[citado 2024 out. 05 ] Available from: https://doi.org/10.1016/j.lithos.2014.07.023

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