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Early exhumation of high‐pressure rocks in extrusion wedges: Cycladic blueschist unit in the eastern Aegean, Greece, and Turkey

Identifieur interne : 009173 ( Main/Exploration ); précédent : 009172; suivant : 009174

Early exhumation of high‐pressure rocks in extrusion wedges: Cycladic blueschist unit in the eastern Aegean, Greece, and Turkey

Auteurs : Uwe Ring [Nouvelle-Zélande] ; Thomas Will [Allemagne] ; Johannes Glodny [Allemagne] ; Christine Kumerics [Allemagne] ; Klaus Gessner [Australie] ; Stuart Thomson [États-Unis] ; Talip Güngör [Turquie] ; Patrick Monié [France] ; Martin Okrusch [Allemagne] ; Kirsten Drüppel [Allemagne]

Source :

RBID : ISTEX:ECC15FE2A7DD1DFF9B410790EFBACFF1DC1DEB71

Descripteurs français

English descriptors

Abstract

Structural, metamorphic, and geochronologic work shows that the Ampelos/Dilek nappe of the Cycladic blueschist unit in the eastern Aegean constitutes a wedge of high‐pressure rocks extruded during early stages of orogeny. The extrusion wedge formed during the incipient collision of the Anatolian microcontinent with Eurasia when subduction and deep underthrusting ceased and the Ampelos/Dilek nappe was thrust southward over the greenschist‐facies Menderes nappes along its lower tectonic contact, the Cycladic‐Menderes thrust, effectively cutting out a ∼30‐ to 40‐km‐thick section of crust. The upper contact of the Ampelos/Dilek extrusion wedge is the top‐to‐the‐NE Selçuk normal shear zone, along which the Ampelos/Dilek nappe was exhumed by ∼30–40 km. Detailed Rb‐Sr and 40Ar/39Ar dating of mylonites demonstrates that both shear zones operated between 42 and 32 Ma. There is no evidence for episodic motion during the ∼10 Myr life span of the shear zones, suggesting that both shear zones operated in a steady, nonepisodic fashion. Our data provide supporting evidence that simultaneous thrust‐type and normal sense shearing can accomplish the early exhumation of deep‐seated rocks.

Url:
DOI: 10.1029/2005TC001872


Affiliations:


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Le document en format XML

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<term>Agios nikolaos nappe</term>
<term>Alps</term>
<term>Amph</term>
<term>Amphibole</term>
<term>Anatolian microcontinent</term>
<term>Apatite</term>
<term>Apparent ages</term>
<term>Assemblage</term>
<term>Basal</term>
<term>Biotite</term>
<term>Blueschist</term>
<term>Catlos</term>
<term>Central aegean</term>
<term>Chlorite</term>
<term>Chloritoid</term>
<term>Cooling ages</term>
<term>Cretan detachment</term>
<term>Cyclades</term>
<term>Cycladic</term>
<term>Cycladic blueschist unit</term>
<term>Decompression</term>
<term>Deep underthrusting</term>
<term>Deformation</term>
<term>Dilek</term>
<term>Dilek nappe</term>
<term>Ductile</term>
<term>Ductile deformation</term>
<term>Dynamic recrystallization</term>
<term>Early exhumation</term>
<term>Earth planet</term>
<term>Eastern aegean</term>
<term>Eastern alps</term>
<term>Eastern mediterranean</term>
<term>Eocene</term>
<term>Epidote</term>
<term>Evia island</term>
<term>Exhumation</term>
<term>Exhumation processes</term>
<term>External hellenides</term>
<term>Extrusion</term>
<term>Extrusion wedge</term>
<term>Extrusion wedges</term>
<term>Fluid flow</term>
<term>Foliation</term>
<term>Garnet</term>
<term>Geochronologic work</term>
<term>Geochronology</term>
<term>Geoforschungszentrum potsdam</term>
<term>Geol</term>
<term>Gessner</term>
<term>Glodny</term>
<term>Grain size</term>
<term>Greater himalayan</term>
<term>Grujic</term>
<term>Hellenides</term>
<term>Himalayan</term>
<term>Hornblende</term>
<term>Increment</term>
<term>Isotope</term>
<term>Isotopic</term>
<term>Kbar</term>
<term>Kyanite</term>
<term>Laser</term>
<term>Late cretaceous</term>
<term>Late eocene</term>
<term>Late eocene extrusion wedge</term>
<term>Latest increments</term>
<term>Lycian</term>
<term>Lycian nappes</term>
<term>Massive metagabbros</term>
<term>Maximum ages</term>
<term>Menderes</term>
<term>Menderes nappes</term>
<term>Metagabbro</term>
<term>Metagabbros</term>
<term>Metamorphic</term>
<term>Metamorphism</term>
<term>Mica</term>
<term>Mica crystals</term>
<term>Mica grains</term>
<term>Mineral assemblages</term>
<term>Miocene</term>
<term>Muscovite</term>
<term>Mylonite</term>
<term>Mylonites</term>
<term>Mylonitic</term>
<term>Mylonitic deformation</term>
<term>Mylonitic rocks</term>
<term>Mylonitization</term>
<term>Mylonitized metagabbros</term>
<term>Nappe</term>
<term>Nappes</term>
<term>Note relic</term>
<term>Paragonite</term>
<term>Petrol</term>
<term>Phengite</term>
<term>Plagioclase</term>
<term>Progressive deformation</term>
<term>Quartz</term>
<term>Recrystallization</term>
<term>Recrystallized</term>
<term>Reddy</term>
<term>Reischmann</term>
<term>Samos</term>
<term>Samos island</term>
<term>Schist</term>
<term>Selcuk</term>
<term>Selcuk nappe</term>
<term>Shear sense</term>
<term>Shear zone</term>
<term>Shear zones</term>
<term>Single grains</term>
<term>Solid solution</term>
<term>Spot fusion ages</term>
<term>Subduction</term>
<term>Tectonic</term>
<term>Tectonics</term>
<term>Tibetan detachment</term>
<term>Upper contact</term>
<term>Wedge</term>
<term>Western turkey</term>
<term>White mica</term>
<term>White mica fractions</term>
<term>White mica recrystallization</term>
<term>White micas</term>
<term>Zone</term>
</keywords>
<keywords scheme="Teeft" xml:lang="en">
<term>Agios nikolaos nappe</term>
<term>Alps</term>
<term>Amph</term>
<term>Amphibole</term>
<term>Anatolian microcontinent</term>
<term>Apatite</term>
<term>Apparent ages</term>
<term>Assemblage</term>
<term>Basal</term>
<term>Biotite</term>
<term>Blueschist</term>
<term>Catlos</term>
<term>Central aegean</term>
<term>Chlorite</term>
<term>Chloritoid</term>
<term>Cooling ages</term>
<term>Cretan detachment</term>
<term>Cyclades</term>
<term>Cycladic</term>
<term>Cycladic blueschist unit</term>
<term>Decompression</term>
<term>Deep underthrusting</term>
<term>Deformation</term>
<term>Dilek</term>
<term>Dilek nappe</term>
<term>Ductile</term>
<term>Ductile deformation</term>
<term>Dynamic recrystallization</term>
<term>Early exhumation</term>
<term>Earth planet</term>
<term>Eastern aegean</term>
<term>Eastern alps</term>
<term>Eastern mediterranean</term>
<term>Eocene</term>
<term>Epidote</term>
<term>Evia island</term>
<term>Exhumation</term>
<term>Exhumation processes</term>
<term>External hellenides</term>
<term>Extrusion</term>
<term>Extrusion wedge</term>
<term>Extrusion wedges</term>
<term>Fluid flow</term>
<term>Foliation</term>
<term>Garnet</term>
<term>Geochronologic work</term>
<term>Geochronology</term>
<term>Geoforschungszentrum potsdam</term>
<term>Geol</term>
<term>Gessner</term>
<term>Glodny</term>
<term>Grain size</term>
<term>Greater himalayan</term>
<term>Grujic</term>
<term>Hellenides</term>
<term>Himalayan</term>
<term>Hornblende</term>
<term>Increment</term>
<term>Isotope</term>
<term>Isotopic</term>
<term>Kbar</term>
<term>Kyanite</term>
<term>Laser</term>
<term>Late cretaceous</term>
<term>Late eocene</term>
<term>Late eocene extrusion wedge</term>
<term>Latest increments</term>
<term>Lycian</term>
<term>Lycian nappes</term>
<term>Massive metagabbros</term>
<term>Maximum ages</term>
<term>Menderes</term>
<term>Menderes nappes</term>
<term>Metagabbro</term>
<term>Metagabbros</term>
<term>Metamorphic</term>
<term>Metamorphism</term>
<term>Mica</term>
<term>Mica crystals</term>
<term>Mica grains</term>
<term>Mineral assemblages</term>
<term>Miocene</term>
<term>Muscovite</term>
<term>Mylonite</term>
<term>Mylonites</term>
<term>Mylonitic</term>
<term>Mylonitic deformation</term>
<term>Mylonitic rocks</term>
<term>Mylonitization</term>
<term>Mylonitized metagabbros</term>
<term>Nappe</term>
<term>Nappes</term>
<term>Note relic</term>
<term>Paragonite</term>
<term>Petrol</term>
<term>Phengite</term>
<term>Plagioclase</term>
<term>Progressive deformation</term>
<term>Quartz</term>
<term>Recrystallization</term>
<term>Recrystallized</term>
<term>Reddy</term>
<term>Reischmann</term>
<term>Samos</term>
<term>Samos island</term>
<term>Schist</term>
<term>Selcuk</term>
<term>Selcuk nappe</term>
<term>Shear sense</term>
<term>Shear zone</term>
<term>Shear zones</term>
<term>Single grains</term>
<term>Solid solution</term>
<term>Spot fusion ages</term>
<term>Subduction</term>
<term>Tectonic</term>
<term>Tectonics</term>
<term>Tibetan detachment</term>
<term>Upper contact</term>
<term>Wedge</term>
<term>Western turkey</term>
<term>White mica</term>
<term>White mica fractions</term>
<term>White mica recrystallization</term>
<term>White micas</term>
<term>Zone</term>
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<div type="abstract">Structural, metamorphic, and geochronologic work shows that the Ampelos/Dilek nappe of the Cycladic blueschist unit in the eastern Aegean constitutes a wedge of high‐pressure rocks extruded during early stages of orogeny. The extrusion wedge formed during the incipient collision of the Anatolian microcontinent with Eurasia when subduction and deep underthrusting ceased and the Ampelos/Dilek nappe was thrust southward over the greenschist‐facies Menderes nappes along its lower tectonic contact, the Cycladic‐Menderes thrust, effectively cutting out a ∼30‐ to 40‐km‐thick section of crust. The upper contact of the Ampelos/Dilek extrusion wedge is the top‐to‐the‐NE Selçuk normal shear zone, along which the Ampelos/Dilek nappe was exhumed by ∼30–40 km. Detailed Rb‐Sr and 40Ar/39Ar dating of mylonites demonstrates that both shear zones operated between 42 and 32 Ma. There is no evidence for episodic motion during the ∼10 Myr life span of the shear zones, suggesting that both shear zones operated in a steady, nonepisodic fashion. Our data provide supporting evidence that simultaneous thrust‐type and normal sense shearing can accomplish the early exhumation of deep‐seated rocks.</div>
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<country name="Turquie">
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<name sortKey="Gungor, Talip" sort="Gungor, Talip" uniqKey="Gungor T" first="Talip" last="Güngör">Talip Güngör</name>
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<country name="France">
<region name="Occitanie (région administrative)">
<name sortKey="Monie, Patrick" sort="Monie, Patrick" uniqKey="Monie P" first="Patrick" last="Monié">Patrick Monié</name>
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</country>
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   |texte=   Early exhumation of high‐pressure rocks in extrusion wedges: Cycladic blueschist unit in the eastern Aegean, Greece, and Turkey
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