Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Cízia Mara Hercos"'
Autor:
Arthur Antonio Machado, Michel Michaelovitch de Mahiques, Yuri L. Camargo, Cízia Mara Hercos, Bruna Teixeira Pandolpho, Antonio H. F. Klein, Gilmar Vital Bueno, Antonio Fernando H. F. Filho, Yhaohannah Lima, Adriano R. Viana, Carlos Theodoro, Isadora Dutra
A new mixed turbidite-contourite system is described in the northern Campos Basin, southeastern Brazilian margin. This system is developed in a middle slope setting and was formed through non-synchronous interaction between the turbidity current and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b324386decff047fc363468aa703a312
https://doi.org/10.5194/egusphere-egu21-3139
https://doi.org/10.5194/egusphere-egu21-3139
Autor:
Isadora Dutra, Antonio Fernando H. F. Filho, Bruna Teixeira Pandolpho, Antonio H. F. Klein, Gilmar Vital Bueno, Carlos Theodoro, Cízia Mara Hercos, Yuri L. Camargo, Michel Michaelovitch de Mahiques, Arthur Antonio Machado, Adriano R. Viana, Yhaohannah Lima
Publikováno v:
Repositório Institucional da USP (Biblioteca Digital da Produção Intelectual)
Universidade de São Paulo (USP)
instacron:USP
Universidade de São Paulo (USP)
instacron:USP
Highlights • A new description of a non-synchronous Mixed Turbidite-Contourite System. • Alternated and cyclic deposits of down-slope and along-slope processes with a transitional stage of flow interaction. • Dominant flow depositional systems
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::790c7e657b9c460682c86f0f33afa625
https://doi.org/10.1016/j.margeo.2021.106422
https://doi.org/10.1016/j.margeo.2021.106422
Autor:
Cízia Mara Hercos, Marcos Antônio da Silva Silveira, Ana Claudia dos Santos Brasil, Ana Paula da Costa Falcão, Alexandre Tadeu Politano, Adriano R. Viana, Renata Carolina Mikosz Arantes, Guarani de Hollanda Cavalcanti, Maria Patricia Curbelo-Fernandez
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d6ac96b5ca71280614024a0d824253c7
https://doi.org/10.1016/b978-85-352-7295-6.50003-8
https://doi.org/10.1016/b978-85-352-7295-6.50003-8
Autor:
Adriana da Costa Braga, Adriano Roessler Viana, Agnaldo Silva Martins, Alexandre Luiz Neves Borges, Alexandre Tadeu Politano, Ana Claudia dos Santos Brasil, Ana Paula da Costa Falcão, Angelo Fraga Bernardino, Carlos Alberto de Moura Barboza, Cízia Mara Hercos, Elianne Pessoa Omena, Frederico Silva Nunes, Frederico Tapajós de Souza Tâmega, Guarani de Hollanda Cavalcanti, Helena Passeri Lavrado, Ivan Daniel Della Giustina, Livia de Laia Loiola, Manuel Haimovici, Marcia Abreu de Oliveira Figueiredo, Marcos Antônio da Silva Silveira, Maria Carolina Müller de Oliveira Henriques, Maria Patricia Curbelo-Fernandez, Michael Maia Mincarone, Paulo Alberto Silva da Costa, Rafael Bendayan de Moura, Renata Carolina Mikosz Arantes, Renato Oscar Kowsmann, Renato Parkinson Martins, Sergio Rosso, Virgínia Lauria Filgueiras
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::62ae562a787ec0dd8517eba64840dd10
https://doi.org/10.1016/b978-85-352-7295-6.50015-4
https://doi.org/10.1016/b978-85-352-7295-6.50015-4
Autor:
Sinara B. De Andrade, Adriano R. Viana, José Luís Magalhães, Waldemar De Almeida, Cízia Mara Hercos
Publikováno v:
Geological Society, London, Memoirs. 22:249-259
Geophysical and sedimentological data indicate that bottom currents have played a fundamental role in deposition along the Campos continental slope, especially during the Neogene and Quaternary. Sediment drifts are clearly observed in 2D and 3D seism
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6835e7ab6336e540b4c664f32f583fd5
https://doi.org/10.1144/gsl.mem.2002.022.01.18
https://doi.org/10.1144/gsl.mem.2002.022.01.18
Publikováno v:
Repositório Institucional da UFOP
Universidade Federal de Ouro Preto (UFOP)
instacron:UFOP
Universidade Federal de Ouro Preto (UFOP)
instacron:UFOP
A porção leste da Bacia do São Francisco, nos arredores da serra da Água Fria, conta com uma seção sísmica (240-RL-300) de direção NW-SE. Ao longo dessa seção foi possível reconhecer os estilos estruturais dominantes no segmento estudado
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ad5e5a270facd1278f4db2a2a3820980
http://www.repositorio.ufop.br/handle/123456789/999
http://www.repositorio.ufop.br/handle/123456789/999