... and Dirphis border faults on the island of Evvia, central Greece (overstep = 20 km, overlap = 15 km), is much bro- ader and has a saddle-like morphology (Fig. 4). Interference zone. Interference transfer zones (after ter- minology of Versfelt & Rosendahl 1989) are characterized by arrays of dip-slip...

... conditions of the prehnite-pumpellyite facies ( e.g . Mellini et al. , 1984 ). Reinecke (1986) detected sursassite in Mn-rich quartzites on the islands of Andros and Evvia, Greece, with Mg-contents in the range of 0.49 - 0.74 (p.f.u.). At these locations sursassite has formed under blue-schist facies...

... and date the style of faulting in central Greece by combining analysis of 19 offshore seismic lines with onshore structural observations on Syros Island and LA-ICP-MS U-Pb dating of calcite sampled in two major fault zones of Syros (Palos and Fabrika faults). Three main sets of faults have been identified...

... that crosscut the low-grade manganiferous deposit of the Lienne Valley in the southwestern part of the Venn-Stavelot Massif ( Schreyer et al. 1986 ). Two extensively studied piemontite occurrences are from the Islands of Andros and Evvia (Greece) that both belong to the Attic-Cycladic blueschist belt...

... , T. 1986 . Phase relationships of sursassite and other Mn-silicates in highly oxidized low-grade, high-pressure metamorphic rocks from Evvia and Andros Islands, Greece . Contributions to Mineralogy and Petrology 94 , 110 – 26 . Rice , J. M. 1977 . Progressive metamorphisim...

... Pelagonian basement with the Carboniferous intrusives extends from northwestern continental Greece to the southeast Aegean and includes areas such as Chios, Evvia, Attica, Argolis, Hydra, and Kalymnos. The Variscan basement is locally exposed and eroded in small rifts; thus, Verrucano-type siliciclastic...

... high-pressure/low-temperature (HP/LT) sequences in the central part of the Cycladic archipelago and the blueschist-facies rocks that occur on Evvia and mainland Greece. The contrast between lawsonite-bearing high-pressure rocks on Evvia and the epidote-blueschist to eclogite-facies rocks in the central...

.... Nonetheless, these faults are also segmented over distances of less than 10 km. The Gediz graben is thus similar to the Gulf of Corinth, central Greece, in that there is no change in polarity of the major fault along the graben, but differs from the Gulf of Evvia where the polarity does change (Roberts...

... and Evvia islands) . Geodinamica Acta 7 : 57 – 85 . Gautier P , Bosse V , Cherneva Z , Didier A , Gerdjikov I , Tiepolo M . 2017 . Polycyclic alpine orogeny in the Rhodope metamorphic complex: the record in migmatites from the Nestos shear zone (N. Greece...

... is known from the Sanbagawa metamorphic belt in Japan ( Matsubara & Kato, 1987 ; Minakawa & Momoi, 1987 ) and from Akra Bouri in Southern Evvia, Greece (sample Ev86/78; Pasero et al. , 1994 ). In Italy, ardennite-(V) with 3.75–5.13 wt% V 2 O 5 was found in a piemontite-bearing micaschist...

... ( Fig. 1 ). Two metamorphic belts are well documented in the Aegean, from north to south: the Cycladic blueschists formed ca. 40–45 Ma (i.e., grey areas in Fig. 1A ), and the Cretan blueschists are Miocene age (25 Ma; black domains in Fig. 1A ). In the Cyclades, PT data for Evvia (Ev), Tinos (Ti...

...Nikita Bragin; Taniel Danelian; Frank Chanier Abstract Well-preserved Late Norian Radiolaria were extracted from two pebbles of radiolarian chert included in Lower Miocene conglomerates of the Pentalofos Formation, in the area of Meteora (Mesohellenic basin, Greece). Both samples yielded a similar...

.... , Okrusch , M. , Seidel , E. , Kreuzer , H. , Harre , W. , Lenz , H. , Wendt , I. , Wagner , G.A. ( 1979 ): Geochronology of High-Pressure Rocks on Sifnos (Cyclades, Greece) . Contrib. Mineral. Petrol ., 70 , 245 – 255 . Avigad , D. ( 1990 ): Geodynamic evolution...

... in continental Greece and Peloponnesos they trend northwest-southeast with small delay times. Hatzfeld et al. (2001 , p. 30,737) concluded: “Our results, both in fast polarization directions and in values of delay time, do not support the idea that anisotropy is associated with inherited tectonic fabric nor...

..., Evvia (Euböa) and at Apikia, Andros island, Greece ( Reinecke et al. 1991 ). Noélbensonite, a BaMn analogue of lawsonite, occurs as a small inclusion in the abswurmbachite-rich core, and is the second report following the type crystal from Woods mine, Australia ( Kawachi et al. 1996 ). Aggregates...

... for correlation are situated in the eastern Rhodope Massif of Greece and Bulgaria. There, the tectonic pattern is dominated by late Alpine metamorphic culminations, namely the Kesebir–Kardamos and the Byala reka–Kechros domes ( Bonev, 2006 ; Bonev, Burg & Ivanov, 2006 ; Bonev, Marchev & Singer, 2006...

... Society of London Greece drainage sedimentation stratigraphy rift zones References Apostolopoulos, G: 1993. Geophysical studies in the Sperchios basin. PhD thesis, University of Athens (in Greek). Billiris H. Paradissis D. Veis G. England P. Featherstone W...

... belt, with strong shortening in the center of the orocline, e.g., in Alaska ( Johnston, 2001 ), eastern Australia ( Li et al., 2012 ), or Cantabria, Spain ( Pastor-Galan et al., 2015 ; Weil, 2006 ). Extensional oroclines, such as in Calabria, Italy, or the Aegean region, Greece, on the other hand...

... and Bihain, Ardennes, Belgium; Mili, Evvia Island, Greece ( Pasero et al. , 1994 ). According to the accepted definition of mineral, As-dominant and V-dominant ardennite are different species, and deserve two distinct names. Since ardennite is the worldwide accepted name for the As-dominant species, we...