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Timing, kinematics and cause of Aegean extension: a scenario based on a comparison with simple analogue experiments
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
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1999 (English)In: TECTONOPHYSICS, ISSN 0040-1951, Vol. 315, no 1-4, 31-72 p.Article in journal (Refereed) Published
Abstract [en]

Since the early 1970s, most geodynamic models proposed for the Eastern Mediterranean consider that the initiation of extension in the Aegean, during the late Middle Miocene or later, was a direct consequence of the westward extrusion of Anatolia away from

Place, publisher, year, edition, pages
ELSEVIER SCIENCE BV , 1999. Vol. 315, no 1-4, 31-72 p.
Keyword [en]
Aegean; analogue experiments; extension; extrusion; gravity spreading; METAMORPHIC CORE COMPLEX; SOUTHERN MENDERES MASSIF; ACTIVE CRUSTAL DEFORMATION; NORTH ANATOLIAN FAULT; HELLENIC ARC; WESTERN TURKEY; MEDITERRANEAN REGION; GPS MEASUREMENTS; MICROEARTHQ
Identifiers
URN: urn:nbn:se:uu:diva-37707OAI: oai:DiVA.org:uu-37707DiVA: diva2:65606
Note
Addresses: Gautier P, Univ Rennes 1, CNRS UPR 4661, Geosci Rennes, Campus Beaulieu, F-35042 Rennes, France. Univ Rennes 1, CNRS UPR 4661, Geosci Rennes, F-35042 Rennes, France. Uppsala Univ, Inst Earth Sci, Hans Ramberg Tecton Lab, S-75236 Uppsala, SwedenAvailable from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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