skip to main content
Visitante
Meu Espaço
Minha Conta
Sair
Identificação
This feature requires javascript
Tags
Revistas Eletrônicas (eJournals)
Livros Eletrônicos (eBooks)
Bases de Dados
Bibliotecas USP
Ajuda
Ajuda
Idioma:
Inglês
Espanhol
Português
This feature required javascript
This feature requires javascript
Primo Search
Busca Geral
Busca Geral
Acervo Físico
Acervo Físico
Produção Intelectual da USP
Produção USP
Search For:
Clear Search Box
Search in:
Busca Geral
Or select another collection:
Search in:
Busca Geral
Busca Avançada
Busca por Índices
This feature requires javascript
This feature requires javascript
The Cenozoic tectonic evolution of Alpine Corsica
Waters, C. N
Journal of the Geological Society, 1990-09, Vol.147 (5), p.811-824
[Periódico revisado por pares]
London: Geological Society of London
Texto completo disponível
Citações
Citado por
Exibir Online
Detalhes
Resenhas & Tags
Mais Opções
Nº de Citações
This feature requires javascript
Enviar para
Adicionar ao Meu Espaço
Remover do Meu Espaço
E-mail (máximo 30 registros por vez)
Imprimir
Link permanente
Referência
EasyBib
EndNote
RefWorks
del.icio.us
Exportar RIS
Exportar BibTeX
This feature requires javascript
Título:
The Cenozoic tectonic evolution of Alpine Corsica
Autor:
Waters, C. N
Assuntos:
Adria
;
Alps
;
basement
;
basins
;
Bastia
;
blueschist
;
Cenozoic
;
continental crust
;
Corsica
;
crust
;
crustal shortening
;
displacements
;
distribution
;
Earth sciences
;
Earth, ocean, space
;
Eurasian Plate
;
Europe
;
evolution
;
Exact sciences and technology
;
facies
;
faults
;
folds
;
foreland basins
;
France
;
greenschist facies
;
isostasy
;
metamorphic rocks
;
nappes
;
oceanic crust
;
plate collision
;
plate rotation
;
Santo Pietro Group
;
schists
;
slickensides
;
structural geology
;
tectonics
;
Tectonics. Structural geology. Plate tectonics
;
Tenda Massif
;
terranes
;
thrust faults
;
uplifts
;
Western Europe
É parte de:
Journal of the Geological Society, 1990-09, Vol.147 (5), p.811-824
Descrição:
During Palaeocene to Early Oligocene times, hinterland and foreland directed thrusts and folds developed in Alpine Corsica in response to the collision of the European continental plate and oceanic crust adjacent to the Adria promontory. The 'Nappes Supérieures' represent fragments of the oceanic lithosphere, emplaced toward the west upon the Eoalpine Schistes lustrés nappes and Hercynian continental basement. The 'Nappes Supérieures' were unaffected by syn-tectonic metamorphism, whilst the underlying Schistes lustrés nappes developed a greenschist facies replacement of blueschist parageneses and the foreland basement of Hercynian Corsica developed prehnite–pumpellyite facies assemblages. Small flexural basins, occupied by continentally derived flysch deposits, developed at the deformation front and were subsequently overridden by ophiolitic and continental nappes. During Oligocene to Early Miocene times there was a change in deformation style with the generation of strike-slip and normal faults. This non-metamorphic deformation event is considered to result from the 30° anticlockwise rotation of Corso–Sardinia relative to the European plate, producing oceanic lithosphere in the Liguro–Provencal back-arc basin and a zone of collision between Corso–Sardinia and Adria. The rotation of Corsica is modelled as resulting from the indentation of the European continental plate by the Adria microplate.
Editor:
London: Geological Society of London
Idioma:
Inglês
Links
View record in Pascal Francis
This feature requires javascript
This feature requires javascript
Voltar para lista de resultados
Anterior
Resultado
4
Avançar
This feature requires javascript
This feature requires javascript
Buscando em bases de dados remotas. Favor aguardar.
Buscando por
em
scope:(USP_PRODUCAO),scope:(USP_EBOOKS),scope:("PRIMO"),scope:(USP),scope:(USP_EREVISTAS),scope:(USP_FISICO),primo_central_multiple_fe
Mostrar o que foi encontrado até o momento
This feature requires javascript
This feature requires javascript