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<title lang=en>Timing, slip rate, displacement and cooling history of the Mykonos detachment footwall, Cyclades, Greece, and implications for the opening of the Aegean Sea basin</title>
<creator>Brichau, S.</creator>
<creator>Ring, U.</creator>
<creator>Carter, A.</creator>
<creator>Bolhar, R.</creator>
<creator>Monie, Patrick</creator>
<creator>Stockli, D.</creator>
<creator>Brunel, Maurice</creator>
<contributor>School of Earth Sciences, University and Birkbeck College, London ; Université du Québec</contributor>
<contributor>Department of Geological Sciences, University of Canterbury, Christchurch ; Université du Québec</contributor>
<contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor>
<contributor>Department of Geology, University of Kansas, Lawrence ; Université du Québec</contributor>
<description>International audience</description>
<source>ISSN: 0016-7649</source>
<source>Journal of the Geological Society</source>
<publisher>Geological Society</publisher>
<identifier>hal-00412177</identifier>
<identifier>https://hal.archives-ouvertes.fr/hal-00412177</identifier>
<source>https://hal.archives-ouvertes.fr/hal-00412177</source>
<source>Journal of the Geological Society, Geological Society, 2008, 165, pp.263-277. 〈10.1144/0016-76492006-145〉</source>
<identifier>DOI : 10.1144/0016-76492006-145</identifier>
<relation>info:eu-repo/semantics/altIdentifier/doi/10.1144/0016-76492006-145</relation>
<language>en</language>
<subject lang=en>High-pressure metamorphism</subject>
<subject lang=en>U-Pb geochronology</subject>
<subject lang=en>western Turkey</subject>
<subject lang=en>core complex</subject>
<subject lang=en>shear zone</subject>
<subject lang=en>cretan detachment</subject>
<subject lang=en>zircon standard</subject>
<subject lang=en>northern Chile</subject>
<subject lang=en>nist srm-610</subject>
<subject lang=en>exhumation</subject>
<subject>[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/Tectonics</subject>
<subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject>
<subject>[SDE.MCG] Environmental Sciences/Global Changes</subject>
<type>info:eu-repo/semantics/article</type>
<type>Journal articles</type>
<description lang=en>We constrain the slip and cooling history of the Mykonos detachment footwall using thermochronometry. A U-Pb zircon age of 13.5 +/- 0.3 Ma dates intrusion of the Mykonos monzogranite. Ar-40/ Ar-39 homblende and biotite ages from the monzogranite are 12.7 +/- 0.6 Ma and 10.9 +/- 0.6 Ma, whereas zircon and apatite fission-track ages range from 13 +/- 0.8 Ma to 10.7 +/- 0.8 Ma and 12.5 +/- 2.2 Ma to 10.5 +/- 1.8 Ma. (U-Th)/He ages range from 13.6 +/- 0.6 Ma to 9.0 +/- 0.7 Ma for zircon and 11. +/- 10.5 Ma to 8.9 +/- 0.4 Ma for apatite. The ages in part overlap within 2 sigma errors and together with the long apatite fission-track lengths (>14 mu m) support rapid cooling at rates > 100 degrees C Ma(-1). The low-temperature thermochronometric ages decrease east-northeastwards in the direction of hanging-wall transport on the Mykonos detachment. Age-distance relationships show that the Mykonos detachment slipped at an average rate of 6.0 + 9.2/-2.4 km Ma(-1) c. 30 km of offset and c. 12 km of exhumation. This result indicates that Miocene low-angle normal faulting was not important for the exhumation of the Cycladic blueschist unit. The opening of the Aegean Sea basin in the Miocene was controlled by a few large-magnitude low-angle normal faults.</description>
<date>2008</date>
</dc>
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