Contribution to the structural study of the Rhodiani ophiolites, Vourinos massif
Περίληψη
The Rhodiani area geologically is comprised of a sequence of Mesozoic and Tertiary thrust sheets, including the Jurassic ophiolite and sedimentary covers; they composed of an ultramafic unit overlain by an Albian to Cenomanian redeposited limestone cover, and at the top a volcanic unit that is overlain by neritic to pelagic Upper Jurassic to Upper Cretaceous age limestone and Upper Maastrichtian flysch deposits. These thrust sheets were emplaced over the Pelagonian platform. Therefore the Rhodiani "ophiolite" is not a single thrust unit, but it is an imbricated ophiolite tectonic structure resulting from a two-stage emplacement process; the ultramafic unit was overthrust on the melange of the Pelagonian platform during the initial emplacement (Jurassic) and the volcanic unit was re-thrust on the former during subsequent post-Eocene tectonic phase
Λεπτομέρειες άρθρου
- Πώς να δημιουργήσετε Αναφορές
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PHOTIADES, A., & ΡΟΜΟΝΙ-ΡΑΡΑΙΟΑΝΝΟΥ F. (2001). Contribution to the structural study of the Rhodiani ophiolites, Vourinos massif. Δελτίο της Ελληνικής Γεωλογικής Εταιρείας, 34(1), 111–118. https://doi.org/10.12681/bgsg.16950
- Ενότητα
- Γενική και Τεκτονική Γεωλογία
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Λήψεις
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Αναφορές
ALTHERR, R., SCHLIESTEDT, M., OKRUSCH, M., SEIDEL, E., KRUEZER, H., HARRE, W., LENZ, H., WENDT, J. & WAGNER, GA. (1979): Geochronology of high-pressure rocks on Sifnos (Cyclades, Greece). Contrib. Mineral. Petrol, 70, 245-255.
BECCALUVA, L., OHNENSTETTER, D., OHNENSTETTER, M. & PAUPY, A. (1984): Two magmatic series with island-arc affinity within the Vourinos ophiolite. Contrib. Mineral. Petrol, 85, 253-271.
BONNEAU, M. (1984): Correlation of the Hellenides nappes in southeast Aegean and their tectonic reconstruction. In: DIXON J.E. & ROBERTSON, A.H.F. (Eds.) In: DIXON J.E. & ROBERTSON, A.H.F. (Eds.) The geological evolution of the Eastern Mediterranean. Geol. Soc. London, Spec. Pubi 17,517-528.
BORTOLOTTI, V, CARRAS, Ν., CHIARI, M., FAZZUOLI, M., MARCUCCI, M., PHOTIADES, A. & PRINCIPI, G. (2000): Decline and fall of an Upper Jurassic - Cretaceous carbonate platform, born (possibly) over wedging ophiolites: Vourinos- Pindos area, Northern Greece- Preliminary results. Abstract and Poster for the 80" Riunione estiva della Soc. Geol. Italiana, Trieste, 6-8 Setembre 2000, 93p.
BRUNN, (1956): Etude géologique du Pinde septentrional et de la Macédoine occidentale. Ann. géol. Pays Hellen., 7, 358p.
BRUNN, J.H., FAUGERES, L. & ROBERT, P. (1972): Une nouvelle série du Jurassique moyen - Crétacé inférieur surmontant les ophiolites dans le détroit de Kozani (Macédoine, Grèce). C. R. somm. Soc. géol. France, 1, 26-27.
DOUTSOS, T., KOUKOUVELAS, L, ZELILIDIS, A. & KONTOPOULOS, N. (1994): Intracontinental wedging and post-orogenic collapse in the Mesohellenic trough. Geol. Rundsch. 83, 257-275.
ECONOMOU, M., DIMOU, E., ECONOMOU, G., MIGIROS, G., VACONDIOS, J., GRIVAS, E., RASSIOS, A. & DABITZIAS, S. (1986): Chromite deposits of Greece. Theophrastus publications S.A., Athens, 129-159.
FAUGERES, L. & ROBERT, P. (1969): Précisions nouvelles sur les altérations contenues dans la série du chaînon de Vigla (Kozani, Macédoine, Grèce). C. R. somm. Soc. géol. France, 97-98.
GRIVAS, E., RASSIOS, Α., KONSTANTOPOULOU, G., VACONDIOS, I. & VRAHATIS, G (1993): Drilling for "blind" podiform chrome ore bodies at Voidolakkos in the Vourinos ophiolite complex, Greece. Econ. Geol, 88, 461-468.
JACOBSHAGEN, V, DURR, ST., KOCKEL, F., KOPP, K.O. & KOWALCZYK, G. (1978): Structure and geodynamic evolution of the Aegean region. In Cloos, Roeder and Schmidt (eds.), Alps, Apennines, Hellenides, Scheizerbart'sche Vergagsbuchhandlung, Stuttgart, 537-564.
JONES, G. & ROBERTSON, A.H.F. (1991): Tectono-stratigraphy and evolution of the Mesozoic Pindos ophiolite and related units, northwestern Greece. J. Geol. Soc. London, 148, 267-288.
NAYLOR, M.A. & HARLE, T.J. (1976): Paleogeographic significance of rocks and structures beneath the Vourinos ophiolite Northern Greece. J. Geol. Soc. London, 132, 667-675.
MAVRIDIS, A. & KELEPERTZIS, A. (1993): Geological map of Greece «KNIDHI sheet» in scale 1:50.000. 1GME (Ed.), Athens, Greece.
MAVRIDIS, A. & MATARANGAS, D. (1979): Geological map of Greece «AYIOFILLON sheet» in scale 1:50.000. IGME (Ed.), Athens, Greece.
MAVRIDES, Α., SKOURTSIS-KORONEOU, V. & TSAILA-MONOPOLIS, S. (1977): Contribution to the geology of the Subpelagonian Zone (Vourinos area, West Macedonia): In 6,h Colloquium on the Geology of the Aegean Region. IGME, Athens, 175-195.
MERCIER, J. (1968): Etude géologique des zones internes des Hellénides en Macédoine centrale (Grèce). Ann. géol. Pays Hellen., 20, 1-792.
MOORES, E.G. (1969): Petrology and structure of the Vourinos ophiolite complex of Northern Greece. Geol. Soc. Am., Spec. Paper, 118, 74pp.
MOUNTRAKIS, D. (1984): Structural evolution of the Pelagonian zone in Northwestern Macedonia, Greece. In: DIXON J.E. & ROBERTSON, A.H.F. (Eds.) In: DIXON J.E. & ROBERTSON, A.H.F. (Eds.) The geological evolution of the Eastern Mediterranean. Geol. Soc. London, Spec. Pubi. 17, 581-590.
MOUNTRAKIS, D., KILIAS, A. & ZOUROS, N. (1993): Kinematic analysis and Tertiary evolution of the Pindos - Vourinos ophiolites (Epirus - Western Macedonia, Greece). Bull. Geol. Soc. Greece, 28/1, 111-124.
PAPANIKOLAOU, D. & ZAMBETAKIS-LEKKAS, A. (1980): Nouvelles observations et datation de la base de la série pélagonienne (s.s.) dans la région de Kastoria, Grèce. C. R. Acad. Paris, 291, 155-158.
PAUPY, (1976): Nouvelles données sur un type de différenciation du magma ophiolitique: Le Massif du Vourinos (Grèce).Thèse Université de Nancy, 182p.
PHOTIADES, Α., SKOURTSIS-CORONEOU, V. & GRIGORIS, P. (1998): The stratigraphie and paleogeographic evolution of the eastern Pelagonian margin during the Late Jurassic - Cretaceous interval (Western Vermion Mountain -Western Macedonia, Greece). Bull. Geol. Soc. Greece, 32/1, 71-77.
PICHON, (1977): Une transversale dans la Zone Pélagonienne, depuis les collines de Krapa (SW) jusqu'au massif du Vermion (NE): Les premières séries transgressives sur les ophiolites): In 6!h Colloquium on the Geology of the Aegean Region. IGME, Athens, 163-171.
PICHON, J.F & LYS, M. (1976). Sur l'existence d'une série du Jurassique supérieur à Crétacé inférieur surmontant les ophiolites dans les collines de Krapa (Massif du Vourinos, Grèce). C. R. Acad. Sci., Paris, 282, 523-526.
RASSIOS, Α., BECCALUVA, L., BORTOLOTTI, V, MAVRIDES, A. & MOORES, E. (1983): Vourinos complex: Field guide for workshop on the Vourinos-Guevgueli ophiolites, I.G.C.P. 197. Ofioliti, 8/3, 275-292.
ROBERTS, S., RASSIOS, Α., WRIGHT, L., VACONDIOS, I., VRACHATIS, G., GRIVAS, E. & NESBITT, R. (1988): Structural controls on the location and form of the Vourinos chromite deposits. In Boissonas, J. & Omenetto, P. (eds.), Mineral deposits within the European Community, Soc. Geol. Appi. Min. Deposits, Spec. Pubi., 6, 249-266.
ROBERTSON, A.H.F, CLIFT, P.D., DEGNAN, P.J. & JONES, G. (1991): Palaeogeographic and palaeotectonic evolution of the eastern Mediterranean Neotethys. Palaeo. Palaeo. Palaeo., 87, 289-343.
VERGELY, P. (1977): Discussion of the paleogeographic significance of rocks beneath the Vourinos ophiolite, northern Greece. J. Geol. Soc. London, 133, 505-507.
VERGELY, P. (1984): Tectonique des ophiolites dans les Hellénides internes. Conséquences sur l'évolution des régions téthysiennes occidentales. Thèse d'état Se. Naturelles, Univ. Paris-Sud, 649p., Orsay.
VERGELY, P. & MERCIER, J. (1990): La fenêtre métamorphique de l'Olympe (Macédoine, Grèce); Compression et extension cénozoïques. Bull.Soc.géol.France, 6/5, 819-829.
SMITH, A.G., WOODCOCK, N.H. & NAYLOR, M.A. (1979): The structural evolution of a Mesozoic continental margin, Othris Mountains, Greece. J. Geol. Soc. London, 136, 589-603.
SPRAY, J.G., BEBIEN, J., REX, D.C. & RODDICK, J.C. (1984): Age constraints on the igneous and metamorphic evolution of the Hellenic-Dinaric ophiolites. In: DIXON J.E. & ROBERTSON, A.H.F. (Eds.) The geological evolution of the Eastern Mediterranean. Geol. Soc. London, Spec. Pubi. 17, 619-627.
SPRAY, J.G. & RODDICK, J.C . (1980): Petrology and 40Ar/39Ar geochronology of some Hellenic sub-ophiolite metamorphic rocks. Contrib. Mineral. Petrol., 72, 43-55.
TERRY, J.P. & MERCIER, M. (1971): Sur l'existence d'une série détritique berriasienne intercalée entre la nappe des ophiolites et le flysch Eocène de la nappe du Pinde (Pinde septentrional, Grèce). C. R. somm. Soc. géol. France, 71-73.
ZIMMERMAN, J.Jr. (1972): Emplacement of Vourinos ophiolite complex, Northern Greece. Geol. Soc. Am. Mem. 132, 225-239.
