A major channel system on the North Faeroes margin from side-scan sonar records

J. Taylor; J.A. Dowdeswell; N.H. Kenyon; T. Nielsen; A. Kuijpers; T.C.E. van Weering; M. Ivanov

doi:10.1007/978-3-642-55846-7_22

A major channel system on the North Faeroes margin from side-scan sonar records

J. Taylor, J.A. Dowdeswell, N.H. Kenyon, T. Nielsen, A. Kuijpers, T.C.E. van Weering, M. Ivanov

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

Abstrakt

The North Faeroes margin has been an area of extensive margin inst ability since probably the Eocene (Nielsen and van Weering 1998; van Weering et al. 1998; Taylor et al. 2000). Typically, the products of such large-scale failure result in long run-out depos its spread over the abyssal plain. Large-scale mapping of the North Faeroes margin indicates that this is not the case in this more tectonically active area of the passive North Atlantic marg in (Taylor et al. 2000, this volume). Low to high resolution sidescan sonar data are shown here, charact erizing the channel system that has developed in response to sediment-column instability.

Originalsprog	Engelsk
Titel	European margin sediment dynamics. Side-scan sonar and seismic images
Redaktører	Jürgen Mienert, Philip Weaver
Udgivelsessted	Heidelberg, Germany
Forlag	Springer
Sider	139-144
Antal sider	5
ISBN (Elektronisk)	978-3-642-55846-7
ISBN (Trykt)	978-3-540-42393-5
DOI	https://doi.org/10.1007/978-3-642-55846-7_22
Status	Udgivet - 2003

Programområde

Programområde 3: Energiressourcer

Adgang til dokumentet

10.1007/978-3-642-55846-7_22

Citationsformater

Taylor, J., Dowdeswell, J. A., Kenyon, N. H., Nielsen, T., Kuijpers, A., van Weering, T. C. E., & Ivanov, M. (2003). A major channel system on the North Faeroes margin from side-scan sonar records. I J. Mienert, & P. Weaver (red.), European margin sediment dynamics. Side-scan sonar and seismic images (s. 139-144). Springer. https://doi.org/10.1007/978-3-642-55846-7_22

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title = "A major channel system on the North Faeroes margin from side-scan sonar records",

abstract = "The North Faeroes margin has been an area of extensive margin inst ability since probably the Eocene (Nielsen and van Weering 1998; van Weering et al. 1998; Taylor et al. 2000). Typically, the products of such large-scale failure result in long run-out depos its spread over the abyssal plain. Large-scale mapping of the North Faeroes margin indicates that this is not the case in this more tectonically active area of the passive North Atlantic marg in (Taylor et al. 2000, this volume). Low to high resolution sidescan sonar data are shown here, charact erizing the channel system that has developed in response to sediment-column instability.",

author = "J. Taylor and J.A. Dowdeswell and N.H. Kenyon and T. Nielsen and A. Kuijpers and {van Weering}, T.C.E. and M. Ivanov",

year = "2003",

doi = "10.1007/978-3-642-55846-7_22",

language = "English",

isbn = "978-3-540-42393-5",

pages = "139--144",

editor = "J{\"u}rgen Mienert and Philip Weaver",

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A major channel system on the North Faeroes margin from side-scan sonar records. / Taylor, J.; Dowdeswell, J.A.; Kenyon, N.H. et al.

European margin sediment dynamics. Side-scan sonar and seismic images. red. / Jürgen Mienert; Philip Weaver. Heidelberg, Germany : Springer, 2003. s. 139-144.

Publikation: Bidrag til bog/rapport/konferenceproceedings › Bogkapitel › Forskning › peer review

TY - CHAP

T1 - A major channel system on the North Faeroes margin from side-scan sonar records

AU - Taylor, J.

AU - Dowdeswell, J.A.

AU - Kenyon, N.H.

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AU - Kuijpers, A.

AU - van Weering, T.C.E.

AU - Ivanov, M.

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N2 - The North Faeroes margin has been an area of extensive margin inst ability since probably the Eocene (Nielsen and van Weering 1998; van Weering et al. 1998; Taylor et al. 2000). Typically, the products of such large-scale failure result in long run-out depos its spread over the abyssal plain. Large-scale mapping of the North Faeroes margin indicates that this is not the case in this more tectonically active area of the passive North Atlantic marg in (Taylor et al. 2000, this volume). Low to high resolution sidescan sonar data are shown here, charact erizing the channel system that has developed in response to sediment-column instability.

AB - The North Faeroes margin has been an area of extensive margin inst ability since probably the Eocene (Nielsen and van Weering 1998; van Weering et al. 1998; Taylor et al. 2000). Typically, the products of such large-scale failure result in long run-out depos its spread over the abyssal plain. Large-scale mapping of the North Faeroes margin indicates that this is not the case in this more tectonically active area of the passive North Atlantic marg in (Taylor et al. 2000, this volume). Low to high resolution sidescan sonar data are shown here, charact erizing the channel system that has developed in response to sediment-column instability.

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A major channel system on the North Faeroes margin from side-scan sonar records

Abstrakt

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