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Attic-Cycladic metamorphic belt

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Journal Article
Published: 15 July 2009
Geological Magazine (2009) 146 (5): 732–742.
...ANTHI LIATI; NIKOS SKARPELIS; GEORGIA PE-PIPER Abstract Numerous post-metamorphic Miocene granitoids occur in the area of Lavrion, SE Attica, at the western end of the Attic-Cycladic Belt of the Aegean. U–Pb ion microprobe-dating (SHRIMP) of zircon from a granitoid sill in the hanging-wall...
Journal Article
Published: 01 February 1991
Journal of the Geological Society (1991) 148 (1): 93–103.
.... Geochronology of metamorphic terrains by the 40 Ar- 39 Ar age spectrum method. PhD Thesis, A.N.U., Canberra. Wilbrans J. R. McDougall I. Metamorphic evolution of the Attic Cycladic Metamorphic Belt on Naxos (Cyclades, Greece) utilizing 40Ar– 39Ar age spectrum measurements Journal...
Journal Article
Published: 01 September 2006
Geological Magazine (2006) 143 (5): 609–620.
... in the time of overprinting can be identified across the Cyclades. Furthermore, an attempt is made to identify distinct stages in the metamorphic history of the Makrotantalon unit, and to date the tectonic emplacement onto the Lower unit. The Attic-Cycladic Crystalline Belt is built up by two major...
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Journal Article
Published: 01 August 1995
Journal of the Geological Society (1995) 152 (4): 639–654.
... of the Attic Cycladic Metamorphic Belt on Naxos (Cyclades, Greece) utilizing 40 Ar/ 39 Ar age spectrum measurements Journal of Metamorphic Geology 1988 6 571 594 Wojtal S. Mitra G. Strain hardening and strain softening in fault zones from foreland thrusts Geological Society of America...
Journal Article
Published: 01 January 2009
European Journal of Mineralogy (2009) 21 (1): 133–148.
...Ioannis Baziotis; Alexander Proyer; Evripidis Mposkos Abstract The Upper Tectonic Unit of the Lavrion area is part of the Attic-Cycladic blueschist belt and was affected by high-pressure, low-temperature metamorphism. Blueschists and greenschists occur in the same outcrop and are believed to have...
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Journal Article
Published: 01 March 2006
European Journal of Mineralogy (2006) 18 (2): 207–222.
... Dora Maira, Attic-Cycladic Complex of Sifnos, Tavsanli Zone and Nilüfer area of NW Turkey. In addition, WKM chemical and b 0 data were used from various sources. The new chemical and b 0 data (EMPA and XRPD) allowed us: ( i ) to establish the reference b 0 and chemistry of WKM from HP/LT metapelites...
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Series: Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.272.01.12
EISBN: 9781862395206
...Abstract Abstract Although the role of extensional tectonics in the exhumation of high-pressure metamorphic terranes is widely established, the kinematics of such deformation remains ambiguous. This paper outlines new field data from the Attic-Cycladic blueschist belt that suggest...
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Journal Article
Published: 01 February 2011
The Canadian Mineralogist (2011) 49 (1): 105–116.
... tourmaline schorl structure cristalline fibres de plans de miroir île de Despotiko Grèce Despotiko is a small, uninhabited island located southwest of Antiparos Island, in the Cyclades, Greece ( Fig. 1 ). Geologically, the island belongs to the AtticCycladic Metamorphic Belt ( Dürr et al. 1978...
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Journal Article
Published: 03 February 2011
Geological Magazine (2011) 148 (4): 511–528.
... tectonostratigraphic unit of the Hellenides. Known outcrops roughly delineate an area of c . 30000 km 2 , but most parts of this terrane are submerged below sea level. The AtticCycladic crystalline belt records a complex structural and metamorphic evolution which documents various stages in the closure...
Journal Article
Published: 01 January 2008
Geological Magazine (2008) 145 (1): 1–15.
... islands, which have been extensively studied. These igneous rocks in SE Attica are the most westerly occurrence of a series of Middle to Late Miocene plutons and hypabyssal rocks in the AtticCycladic belt that were emplaced following the peak of Barrovian metamorphism during widespread extension and mid...
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Journal Article
Published: 01 September 2001
Journal of the Geological Society (2001) 158 (5): 769–784.
... that the Anatolide belt in western Turkey formed under greenschist facies metamorphic conditions in the Eocene when a high-pressure metamorphic fragment of the Adriatic plate (the Cycladic blueschist unit) was thrust onto the imbricated mid-crustal units of the Anatolian microcontinent (the Menderes nappes...
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Journal Article
Published: 19 July 2013
Geological Magazine (2014) 151 (3): 430–446.
... 142 Mills Road, 0200 Canberra, ACT, Australia Makrotantalon Unit Andros Cyclades Attic-Cycladic Crystalline Belt Greece Rb–Sr geochronology † Author for correspondence: magda.huyskens@anu.edu.au 10 09 2012 20 03 2013 Copyright © Cambridge University Press 2013 2013...
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Journal Article
Journal: Geology
Published: 01 March 2002
Geology (2002) 30 (3): 235–238.
.... , and Hohndorf , A. , 1982 , A late Oligocene/early Miocene high temperature belt in the Attic-Cycladic crystalline complex (SE Pelagonian, Greece) : Geologisches Jahrbuch , v. E23 p. 97 – 164 . Andriessen , P.A.M. , Boelrijk , N.A.I.M. , Hebeda , E.H. , Priem , H.N.A. , Verdurmen...
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Journal Article
Journal: Lithosphere
Publisher: GSW
Published: 01 February 2012
Lithosphere (2012) 4 (1): 23–39.
... shear zones. Note the pervasive brittle fracturing of the quartz layer (E Kythnos, 4141812N, 276495E). The rocks of the Cycladic Blueschist unit were exhumed in two successive stages corresponding to two metamorphic episodes ( Jolivet and Brun, 2010 , and references therein), with the first stage...
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Journal Article
Journal: GSA Bulletin
Published: 01 January 2017
GSA Bulletin (2017) 129 (1-2): 93–117.
... history of Attic-Cycladic Belt includes Meso-Hellenic high-pressure metamorphism (M1) mainly at ca. 45 Ma (and ages as old as 116 Ma; Huet et al., 2015 ) and Neo-Hellenic Barrovian-type metamorphism (M2) at greenschist facies to local amphibolite facies (on Naxos) overprinting high-pressure rocks. M1...
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Journal Article
Published: 01 January 2002
Journal of the Geological Society (2002) 159 (1): 45–60.
... and reveal the nature of the overburden that covered the Cycladic blueschist belt during Alpine orogeny in the Tertiary. Abundant metamorphic clasts yielding mica cooling ages between 80 and 100 Ma occur throughout the sedimentary section and probably pertain to a vast Pelagonian-type rock mass that covered...
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Journal Article
Published: 01 May 2003
Geological Magazine (2003) 140 (3): 245–252.
... , A. 1982 . A late Oligocene/early Miocene high temperature belt in the Attic-Cycladic crystalline complex (SE Pelagonian, Greece) . Geologisches Jahrbuch E23 , 97 – 164 . Avigad , D. & Garfunkel , T. 1989 . Low-angle faults above and below a blueschist belt–Tinos Island, Cyclades...
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Journal Article
Published: 01 May 2010
Journal of the Geological Society (2010) 167 (3): 475–489.
.... They are mainly high-K calc-alkaline trachyandesites. Based on their Sr–Nd–Pb isotopic compositions, the mantle source of the Volos–Evia area lavas is similar to that of a large volcanic belt that developed north of the Pelagonian–AtticCycladic–Menderes massifs, encompassing a 35 Ma timespan and widespread over...
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Journal Article
Published: 01 July 2000
Geological Magazine (2000) 137 (4): 367–380.
.... , Kreuzer , H. , Matthews , A. & Okrusch , M. 1993 . 40 Ar/ 39 Ar and oxygen isotope studies of poly-metamorphism from Tinos Island, Cycladic blueschist belt, Greece . Journal of Metamorphic Geology 11 , 223 – 40 . Brocker , M. & Enders , M. 1999 . U–Pb zircon...
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Journal Article
Published: 01 January 2008
Journal of the Geological Society (2008) 165 (1): 263–277.
... sediments ( Le Pichon & Angelier 1979 ). The Cycladic blueschist unit experienced at least two episodes of metamorphism during the Tertiary: an Eocene eclogite- to blueschist-facies metamorphism at 400–550 °C and 12–20 kbar that was followed by at least one greenschist- to amphibolite-facies...
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