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Timing, slip rate, displacement and cooling history of the Mykonos detachment footwall, Cyclades, Greece, and implications for the opening of the Aegean Sea basin

Stéphanie Brichau, Uwe Ring, Andrew Carter, Robert Bolhar, Patrick Monié, Daniel Stockli and Maurice Brunel
Journal of the Geological Society, 165, 263-277, 14 January 2008, https://doi.org/10.1144/0016-76492006-145
Stéphanie Brichau
1School of Earth Sciences, University and Birkbeck College, London WC1E 7HX, UK (e-mail: )
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Uwe Ring
2Department of Geological Sciences, University of Canterbury, Christchurch 8140, New Zealand
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Andrew Carter
1School of Earth Sciences, University and Birkbeck College, London WC1E 7HX, UK (e-mail: )
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Robert Bolhar
2Department of Geological Sciences, University of Canterbury, Christchurch 8140, New Zealand
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Patrick Monié
3UMR 5573, Université Montpellier II, 34095 Montpellier Cedex 05, France
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Daniel Stockli
4Department of Geology, University of Kansas, Lawrence, KS 66045, USA
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Maurice Brunel
3UMR 5573, Université Montpellier II, 34095 Montpellier Cedex 05, France
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Abstract

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. 40Ar/39Ar hornblende 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 11.1 ± 0.5 Ma to 8.9 ± 0.4 Ma for apatite. The ages in part overlap within 2σ errors and together with the long apatite fission-track lengths (>14 μm) support rapid cooling at rates >100 °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 causing 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.

  • © 2008 The Geological Society of London
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Journal of the Geological Society: 165 (1)
Journal of the Geological Society
Volume 165, Issue 1
January 2008
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Timing, slip rate, displacement and cooling history of the Mykonos detachment footwall, Cyclades, Greece, and implications for the opening of the Aegean Sea basin

Stéphanie Brichau, Uwe Ring, Andrew Carter, Robert Bolhar, Patrick Monié, Daniel Stockli and Maurice Brunel
Journal of the Geological Society, 165, 263-277, 14 January 2008, https://doi.org/10.1144/0016-76492006-145
Stéphanie Brichau
1School of Earth Sciences, University and Birkbeck College, London WC1E 7HX, UK (e-mail: )
  • Find this author on Google Scholar
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Uwe Ring
2Department of Geological Sciences, University of Canterbury, Christchurch 8140, New Zealand
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Andrew Carter
1School of Earth Sciences, University and Birkbeck College, London WC1E 7HX, UK (e-mail: )
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Robert Bolhar
2Department of Geological Sciences, University of Canterbury, Christchurch 8140, New Zealand
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Patrick Monié
3UMR 5573, Université Montpellier II, 34095 Montpellier Cedex 05, France
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Daniel Stockli
4Department of Geology, University of Kansas, Lawrence, KS 66045, USA
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Maurice Brunel
3UMR 5573, Université Montpellier II, 34095 Montpellier Cedex 05, France
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Timing, slip rate, displacement and cooling history of the Mykonos detachment footwall, Cyclades, Greece, and implications for the opening of the Aegean Sea basin

Stéphanie Brichau, Uwe Ring, Andrew Carter, Robert Bolhar, Patrick Monié, Daniel Stockli and Maurice Brunel
Journal of the Geological Society, 165, 263-277, 14 January 2008, https://doi.org/10.1144/0016-76492006-145
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