Modelli di accrezione del margine cileno centro-meridionale

Fanucci Francesco, Vargas Cordero Ivan, Loreto M. Filomena, Tinivella Umberta

Resultado de la investigación: Article

Resumen

The continental margin of central-southern Chile presents some morphostructural features not common among the active margins. The trench, with few exceptions, is filled by an important sedimentary prism. The presence and the characters of this prism strongly condition the accretion process in the downslope. They introduces here some examples of active accretion and the cases are discussed in which this process seems to be inactive.

Idioma originalItalian
Páginas (desde-hasta)93-94
Número de páginas2
PublicaciónRendiconti Online Societa Geologica Italiana
Volumen5
EstadoPublished - 2009

Huella dactilar

trench
continental margin
accretion
active margin

ASJC Scopus subject areas

  • Geology

Citar esto

Francesco, Fanucci ; Ivan, Vargas Cordero ; Filomena, Loreto M. ; Umberta, Tinivella. / Modelli di accrezione del margine cileno centro-meridionale. En: Rendiconti Online Societa Geologica Italiana. 2009 ; Vol. 5. pp. 93-94.
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Modelli di accrezione del margine cileno centro-meridionale. / Francesco, Fanucci; Ivan, Vargas Cordero; Filomena, Loreto M.; Umberta, Tinivella.

En: Rendiconti Online Societa Geologica Italiana, Vol. 5, 2009, p. 93-94.

Resultado de la investigación: Article

TY - JOUR

T1 - Modelli di accrezione del margine cileno centro-meridionale

AU - Francesco, Fanucci

AU - Ivan, Vargas Cordero

AU - Filomena, Loreto M.

AU - Umberta, Tinivella

PY - 2009

Y1 - 2009

N2 - The continental margin of central-southern Chile presents some morphostructural features not common among the active margins. The trench, with few exceptions, is filled by an important sedimentary prism. The presence and the characters of this prism strongly condition the accretion process in the downslope. They introduces here some examples of active accretion and the cases are discussed in which this process seems to be inactive.

AB - The continental margin of central-southern Chile presents some morphostructural features not common among the active margins. The trench, with few exceptions, is filled by an important sedimentary prism. The presence and the characters of this prism strongly condition the accretion process in the downslope. They introduces here some examples of active accretion and the cases are discussed in which this process seems to be inactive.

KW - Accretion

KW - Chile trench

KW - Continental margin

KW - Downslope

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EP - 94

JO - Rendiconti Online Societa Geologica Italiana

JF - Rendiconti Online Societa Geologica Italiana

SN - 2035-8008

ER -