Distribución del espesor sedimentario en las cuencas Protector y Pirie (Mar de Scotia, Antártida): factores de control

Lara F. Pérez; F. Javier Hernandez-Molina; Fernando Bohoyo; Andrés Maldonado; Juan T. Vázquez; Francisco J. Lobo; Yasmina M. Martos

Distribución del espesor sedimentario en las cuencas Protector y Pirie (Mar de Scotia, Antártida): factores de control

Lara F. Pérez, F. Javier Hernandez-Molina, Fernando Bohoyo, Andrés Maldonado, Juan T. Vázquez, Francisco J. Lobo, Yasmina M. Martos

Publikation: Bidrag til tidsskrift › Konferenceartikel i tidsskrift › peer review

Resumé

The analysis of multichannel seismic profiles reveals that the distribution of sedimentary depocenters within the Protector and Pirie basins of the southern Scotia Sea, close to the Scotia-Antarctica plate boundary, is largely due to the morpho-structural control of the basement and influenced by the distribution of bottom currents. Both basins constituted a good example of small isolated and undernourished deep basins, lacking major continental inputs and under the influence of active bottom currents related to both the Antarctic Circumpolar deep Water and the Weddell Sea Deep Water.

Originalsprog	Spansk
Sider (fra-til)	133-136
Antal sider	4
Tidsskrift	Geogaceta
Vol/bind	50
Udgave nummer	2
Status	Udgivet - 2011
Udgivet eksternt	Ja
Begivenhed	50 Sesión Científica - Vigo, Spanien Varighed: 27 maj 2011 → 27 maj 2011 Konferencens nummer: 50

Programområde

Programområde 2: Vandressourcer

FN’s Verdensmål

Dette resultat bidrager til følgende verdensmål

Adgang til dokumentet

https://sge.usal.es/archivos/geogacetas/geo50/art31.pdfLicens: Ikke-specificeret

Citationsformater

@article{27ec9145cd8844b2b280f1b2b176a6ff,

title = "Distribuci{\'o}n del espesor sedimentario en las cuencas Protector y Pirie (Mar de Scotia, Ant{\'a}rtida): factores de control",

abstract = "The analysis of multichannel seismic profiles reveals that the distribution of sedimentary depocenters within the Protector and Pirie basins of the southern Scotia Sea, close to the Scotia-Antarctica plate boundary, is largely due to the morpho-structural control of the basement and influenced by the distribution of bottom currents. Both basins constituted a good example of small isolated and undernourished deep basins, lacking major continental inputs and under the influence of active bottom currents related to both the Antarctic Circumpolar deep Water and the Weddell Sea Deep Water.",

author = "P{\'e}rez, \{Lara F.\} and Hernandez-Molina, \{F. Javier\} and Fernando Bohoyo and Andr{\'e}s Maldonado and V{\'a}zquez, \{Juan T.\} and Lobo, \{Francisco J.\} and Martos, \{Yasmina M.\}",

year = "2011",

language = "Spansk",

volume = "50",

pages = "133--136",

journal = "Geogaceta",

issn = "0213-683X",

publisher = "Sociedad Geologica de Espana",

number = "2",

note = "50 Sesi{\'o}n Cient{\'i}fica ; Conference date: 27-05-2011 Through 27-05-2011",

}

TY - JOUR

T1 - Distribución del espesor sedimentario en las cuencas Protector y Pirie (Mar de Scotia, Antártida): factores de control

AU - Pérez, Lara F.

AU - Hernandez-Molina, F. Javier

AU - Bohoyo, Fernando

AU - Maldonado, Andrés

AU - Vázquez, Juan T.

AU - Lobo, Francisco J.

AU - Martos, Yasmina M.

N1 - Conference code: 50

PY - 2011

Y1 - 2011

N2 - The analysis of multichannel seismic profiles reveals that the distribution of sedimentary depocenters within the Protector and Pirie basins of the southern Scotia Sea, close to the Scotia-Antarctica plate boundary, is largely due to the morpho-structural control of the basement and influenced by the distribution of bottom currents. Both basins constituted a good example of small isolated and undernourished deep basins, lacking major continental inputs and under the influence of active bottom currents related to both the Antarctic Circumpolar deep Water and the Weddell Sea Deep Water.

AB - The analysis of multichannel seismic profiles reveals that the distribution of sedimentary depocenters within the Protector and Pirie basins of the southern Scotia Sea, close to the Scotia-Antarctica plate boundary, is largely due to the morpho-structural control of the basement and influenced by the distribution of bottom currents. Both basins constituted a good example of small isolated and undernourished deep basins, lacking major continental inputs and under the influence of active bottom currents related to both the Antarctic Circumpolar deep Water and the Weddell Sea Deep Water.

M3 - Konferenceartikel i tidsskrift

SN - 0213-683X

VL - 50

SP - 133

EP - 136

JO - Geogaceta

JF - Geogaceta

IS - 2

T2 - 50 Sesión Científica

Y2 - 27 May 2011 through 27 May 2011

ER -