Holocene displacement field at an emerged oceanic transform-ridge junction: The Husavik-Flatey Fault – Gudfinnugja Fault system, North Iceland-Reference-Cited by-同舟云学术

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Holocene displacement field at an emerged oceanic transform-ridge junction: The Husavik-Flatey Fault – Gudfinnugja Fault system, North Iceland

Published:2015-06 Issue: Volume:75 Page:118-134
ISSN:0191-8141
Container-title:Journal of Structural Geology
language:en
Short-container-title:Journal of Structural Geology

Author:

Pasquarè Mariotto F.,Bonali F.L.,Tibaldi A.^ORCID,Rust D.^ORCID,Oppizzi P.,Cavallo A.

Publisher

Elsevier BV

Subject

Geology

Reference59 articles.

1. Relevance of Afar seismicity and volcanism to the mechanics of accreting plate boundaries;Abdallah;Nature,1979

2. Interaction and linkage of extension fractures and normal faults: examples from the rift zone of Iceland;Acocella;J. Struct. Geol.,2000

3. Effective tension-shear relationship in extensional fissure swarm, axial rift zone of northeastern Iceland;Angelier;J. Struct. Geol.,1997

4. Variable coupling explains complex tectonic regimes near oceanic transform fault: Flateyjarskagi, Iceland;Angelier;Terra Nova,2000

5. Glacial rebound and plate spreading: results from the first countrywide GPS observations in Iceland;Árnadóttir;Geophys. J. Int.,2009

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