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  • 2005-2009  (2)
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  • 1
    Online Resource
    Online Resource
    Gauge symmetry, t-duality and doubled geometry (2007)
    Hamburg : DESY
    Details Availability
    Keywords: Forschungsbericht
    Type of Medium: Online Resource
    Pages: Online-Ressource (17 S., 293 KB) , graph. Darst.
    Edition: v1, 29 Nov 2007
    Series Statement: DESY 07,189
    URL: https://edocs.tib.eu/files/e01fn09/607470038.pdf
    URL: https://edocs.tib.eu/files/e01fn09/607470038l.pdf
    Language: English
    Note: Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Auch als gedr. Ausg. vorhanden , Systemvoraussetzungen: Acrobat reader.
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  • 2
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    Dalrymple Trough: an active oblique-slip ocean-continent boundary in the northwest Indian Ocean (2008)
    Elsevier
    In:  Earth and Planetary Science Letters, 272 . pp. 437-445.
    Details
    Publication Date: 2019-09-23
    Description: The Dalrymple Trough marks part of the transform plate boundary between India and Arabia in the northern Arabian Sea. Oblique extension is presently active across this portion of the boundary at a rate of a few millimetres per year, and seismic reflection profiles across the trough confirm that it is an extensional structure. We present new swath bathymetric and wide-angle seismic data from the trough. The bathymetric data show that the trough is bounded by a single, steep, 3-km-high scarp to the southeast and a series of smaller, en-echelon scarps to the northwest. Wide-angle seismic data show that a typical oceanic crustal velocity structure is present to the northwest, with a crustal thickness of ~ 6 km. There is an abrupt change in crustal thickness and velocity structure at the northwestern edge of the trough, and the trough itself is underlain by 12-km-thick crust interpreted as thinned continental crust. Therefore we infer that Dalrymple Trough is an unusual obliquely extending plate boundary at which continental crust and oceanic crust are juxtaposed. The extensional deformation is focused on a single major fault in the continental lithosphere, but distributed over a region ~ 60 km wide in the oceanic lithosphere
    Type: Article , PeerReviewed
    Format: text
    DOI: 10.1016/j.epsl.2008.05.007
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    OceanRep: Article in a Scientific Journal - peer-reviewed
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