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Artigo de periodico
Comparing ray-theoretical and finite-frequency teleseismic traveltimes: implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle (2021)
Chaves, Carlos Alberto Moreno ; Ritsema, Jeroen ; Koelemeijer, Paula
Source: Geophysical Journal International. Unidade: IAG
Subjects: SISMICIDADE, MANTO DA TERRA, ONDAS SÍSMICAS
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
CHAVES, Carlos Alberto Moreno e RITSEMA, Jeroen e KOELEMEIJER, Paula. Comparing ray-theoretical and finite-frequency teleseismic traveltimes: implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle. Geophysical Journal International, v. 224, n. 3, p. 1540-1552, 2021Tradução . . Disponível em: https://doi.org/10.1093/gji/ggaa534. Acesso em: 07 set. 2024.
APA
Chaves, C. A. M., Ritsema, J., & Koelemeijer, P. (2021). Comparing ray-theoretical and finite-frequency teleseismic traveltimes: implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle. Geophysical Journal International, 224( 3), 1540-1552. doi:10.1093/gji/ggaa534
NLM
Chaves CAM, Ritsema J, Koelemeijer P. Comparing ray-theoretical and finite-frequency teleseismic traveltimes: implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle [Internet]. Geophysical Journal International. 2021 ; 224( 3): 1540-1552.[citado 2024 set. 07 ] Available from: https://doi.org/10.1093/gji/ggaa534
Vancouver
Chaves CAM, Ritsema J, Koelemeijer P. Comparing ray-theoretical and finite-frequency teleseismic traveltimes: implications for constraining the ratio of S-wave to P-wave velocity variations in the lower mantle [Internet]. Geophysical Journal International. 2021 ; 224( 3): 1540-1552.[citado 2024 set. 07 ] Available from: https://doi.org/10.1093/gji/ggaa534
Artigo de periodico
Giant Gaussian process models of geomagnetic palaeosecular variation: a directional outlook (2020)
Brandt, Daniele ; Constable, Catherine ; Ernesto, Márcia
Source: Geophysical Journal International. Unidade: IAG
Subjects: PALEOMAGNETISMO, GEOMAGNETISMO, ESTATÍSTICA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
BRANDT, Daniele e CONSTABLE, Catherine e ERNESTO, Márcia. Giant Gaussian process models of geomagnetic palaeosecular variation: a directional outlook. Geophysical Journal International, v. 222, n. 3, p. 1526-1541, 2020Tradução . . Disponível em: https://doi.org/10.1093/gji/ggaa258. Acesso em: 07 set. 2024.
APA
Brandt, D., Constable, C., & Ernesto, M. (2020). Giant Gaussian process models of geomagnetic palaeosecular variation: a directional outlook. Geophysical Journal International, 222( 3), 1526-1541. doi:10.1093/gji/ggaa258
NLM
Brandt D, Constable C, Ernesto M. Giant Gaussian process models of geomagnetic palaeosecular variation: a directional outlook [Internet]. Geophysical Journal International. 2020 ; 222( 3): 1526-1541.[citado 2024 set. 07 ] Available from: https://doi.org/10.1093/gji/ggaa258
Vancouver
Brandt D, Constable C, Ernesto M. Giant Gaussian process models of geomagnetic palaeosecular variation: a directional outlook [Internet]. Geophysical Journal International. 2020 ; 222( 3): 1526-1541.[citado 2024 set. 07 ] Available from: https://doi.org/10.1093/gji/ggaa258
Artigo de periodico
Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography (2020)
Portner, Daniel Evan ; Rodríguez, Emily E; Beck, Susan; Zandt, George; Scire, Alissa; Rocha, Marcelo P ; Bianchi, Marcelo Belentani de ; Ruiz, Mario; França, George Sand ; Condori, Cristobal ; Alvarado, Patricia
Source: Journal of Geophysical Research: Solid Earth. Unidade: IAG
Subjects: SISMOLOGIA, TOMOGRAFIA, MANTO DA TERRA
A citação é gerada automaticamente e pode não estar totalmente de acordo com as normas
ABNT
PORTNER, Daniel Evan et al. Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography. Journal of Geophysical Research: Solid Earth, v. 125, n. 5, 2020Tradução . . Disponível em: https://doi.org/10.1029/2019JB017884. Acesso em: 07 set. 2024.
APA
Portner, D. E., Rodríguez, E. E., Beck, S., Zandt, G., Scire, A., Rocha, M. P., et al. (2020). Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography. Journal of Geophysical Research: Solid Earth, 125( 5). doi:10.1029/2019JB017884
NLM
Portner DE, Rodríguez EE, Beck S, Zandt G, Scire A, Rocha MP, Bianchi MB de, Ruiz M, França GS, Condori C, Alvarado P. Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography [Internet]. Journal of Geophysical Research: Solid Earth. 2020 ; 125( 5):[citado 2024 set. 07 ] Available from: https://doi.org/10.1029/2019JB017884
Vancouver
Portner DE, Rodríguez EE, Beck S, Zandt G, Scire A, Rocha MP, Bianchi MB de, Ruiz M, França GS, Condori C, Alvarado P. Detailed Structure of the Subducted Nazca Slab into the Lower Mantle Derived From Continent‐Scale Teleseismic P Wave Tomography [Internet]. Journal of Geophysical Research: Solid Earth. 2020 ; 125( 5):[citado 2024 set. 07 ] Available from: https://doi.org/10.1029/2019JB017884

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