Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Cristina Pierini"'
Publikováno v:
Anuário do Instituto de Geociências, Vol 42, Iss 3, Pp 432-448 (2019)
Foram estabelecidos critérios litoestratigráficos, bioestratigráficos e faciológicos para a caracterização e distinção das seções sedimentares associadas às formações Maceió, Poção e Muribeca (Bacia de Sergipe-Alagoas), com base nas
Externí odkaz:
https://doaj.org/article/c2b96e3115934471828793070eda29e7
Autor:
Nuno Pimentel, Claiton Marlon dos Santos Scherer, Ubiratan Ferrucio Faccini, Cristina Pierini, Ana Maria Pimentel Mizusaki
Publikováno v:
Journal of South American Earth Sciences. 29:412-426
Resumo As paleoalteracoes da Formacao Sergi foram classificadas e estudadas com o objetivo de determinar sua genese e sua relacao com a evolucao estratigrafica. A Formacao Sergi faz parte da sequencia pre-rift da Bacia do Reconcavo (NE Brasil) e e co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::caa7b683735425697a9a18945780ea5e
https://doi.org/10.1016/j.jsames.2009.04.002
https://doi.org/10.1016/j.jsames.2009.04.002
Autor:
Daisy B. Alves, Cristina Pierini, Ana Maria Pimentel Mizusaki, Claiton Marlon dos Santos Scherer
Publikováno v:
Journal of South American Earth Sciences. 15:669-681
Several analytical techniques were applied in the study of the Alemoa Member (Santa Maria formation) and Caturrita formation to make an assessment of changing paleoenvironmental conditions through the Triassic succession of southern Brazil. This incl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5dfd2a9f720863ea76651babed4220c9
https://doi.org/10.1016/s0895-9811(02)00114-1
https://doi.org/10.1016/s0895-9811(02)00114-1
Publikováno v:
Pesquisas em Geociências; v. 34, n. 1 (2007): Pesquisas em Geociências; 45-61
Repositório Institucional da UFRGS
Universidade Federal do Rio Grande do Sul (UFRGS)
instacron:UFRGS
Repositório Institucional da UFRGS
Universidade Federal do Rio Grande do Sul (UFRGS)
instacron:UFRGS
The majority of paleosols are described from continental deposits, most commonly from alluvial strata. In these continental records to much little is revealed of conditions between events of sedimentation. In alluvial sedimentary environments, a reco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1a141b02321a35f9fbfe38e5de2ad7eb
http://seer.ufrgs.br/PesquisasemGeociencias/article/view/19462
http://seer.ufrgs.br/PesquisasemGeociencias/article/view/19462