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Centrifuge modelling of the evolution of low-angle detachment faults from high-angle normal faults
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2001 (English)In: JOURNAL OF STRUCTURAL GEOLOGY, ISSN 0191-8141, Vol. 23, no 8, 1179-1185 p.Article in journal (Refereed) Published
Abstract [en]

Centrifuge models composed of a ductile layer overlain by a semi-brittle layer are used to study how deformation localised by a high-angle normal fault promotes detachment faulting. During lateral extension driven by centrifugal force, localised extension

Place, publisher, year, edition, pages
PERGAMON-ELSEVIER SCIENCE LTD , 2001. Vol. 23, no 8, 1179-1185 p.
Keyword [en]
extension; low-angle detachment; OCT (ocean-continent transition zone); centrifuge models; CONTINENTAL LITHOSPHERE; EXTENSIONAL TECTONICS; CORE COMPLEXES; SYSTEMS; GRAVITY
Identifiers
URN: urn:nbn:se:uu:diva-37853OAI: oai:DiVA.org:uu-37853DiVA: diva2:65752
Note
Addresses: Koyi HA, Uppsala Univ, Dept Earth Sci, Hans RAmberg Tecton Lab, Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, Hans RAmberg Tecton Lab, Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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