Recent and present-day tectonics near a hot spot : the transform zones of iceland

The two transform zones that connect the Icelandic rift segments and the mid-Atlantic Ridge close to the Icelandic hot spot, are described in terms of geometry of faulting and stress fields. They differ in age: 8-8.5 My in the north and 2-3 My in the south, illustrating the different stages of matur...

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Bibliographic Details
Main Authors: Bergerat, Françoise, Angelier, Jacques, Homberg, Catherine, Garcia, Sebastian, Verrier, S., Bellou, Magalie
Other Authors: Institut des Sciences de la Terre de Paris (iSTeP), Université Pierre et Marie Curie - Paris 6 (UPMC)-Centre National de la Recherche Scientifique (CNRS), Géoazur (GEOAZUR 6526), Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Université Nice Sophia Antipolis (1965 - 2019) (UNS)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire de la Côte d'Azur, Université Côte d'Azur (UCA)-Université Côte d'Azur (UCA)-Centre National de la Recherche Scientifique (CNRS), Institut für Geologische Wissenschaften, Freie Universität Berlin
Format: Conference Object
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://hal.univ-brest.fr/hal-00480616
https://hal.univ-brest.fr/hal-00480616/document
https://hal.univ-brest.fr/hal-00480616/file/BergeratF._resume_3_-1.pdf
Description
Summary:The two transform zones that connect the Icelandic rift segments and the mid-Atlantic Ridge close to the Icelandic hot spot, are described in terms of geometry of faulting and stress fields. They differ in age: 8-8.5 My in the north and 2-3 My in the south, illustrating the different stages of maturity in the transform process, from an immature stage illustrated by the South Iceland Seismic Zone to a mature stage shown by the Husavik-Flatey Fault.