Εξώφυλλο

Στοιχεία ενδοωκεάνιας υποβύθισης στο Ελληνικό ορογενές και αναφορές σε διαδικασίες ενδοωκεάνιας υποβύθισης στην Αλπική αλυσίδα και στην ενεργό παγκόσμια γεωδυναμική = Elements of intraoceanic subduction in the Hellenic orogen and references to intraoceanic subduction processes in the Alpine orogenic belt and in the active worldwide geodynamics.

Αγγελική Χρηστάκης Σέλλα

Περίληψη


Στο σύστημα της Τηθύος εξελίχθηκε μια από τις σημαντικότερες ορογενετικές διαδικασίες του πλανήτη, πολύπλοκη και με επιμέρους στάδια, που έδωσε τελικά την Αλπική αλυσίδα, που δομείται από μια σειρά από βουνά. Ξεκινώντας δυτικά από τα όρη του Άτλαντα στην Β. Αφρική, τα Πυρηναία και τις Άλπεις στην Ευρώπη, όπου συνεχίζεται διασπώμενη σε κλάδους στα Απέννινα στην Ιταλία, τις Καρπαθίδες και Διναρίδες στον χώρο της Βαλκανικής, στην οροσειρά της Πίνδου στον κύριο κορμό του Ελληνικού χώρου και σε όλα τα Ελληνικά βουνά, περνώντας στον χώρο της Ασίας στις Ταυρίδες στην Τουρκία, στην Συρία, στο Oman, στα όρη Zagros στο Ιράν, καταλήγει στα Ιμαλάϊα και στα νότια τεμάχη της Κίνας στα ανατολικά.
      Στην προσπάθεια να μελετηθούν οι γεωτεκτονικές διαδικασίες που έλαβαν χώρα στο σύστημα αυτό, οι επιστήμονες που ασχολήθηκαν, προσπάθησαν να εντοπίσουν σημεία που δίνουν σημαντικά στοιχεία για την εξέλιξή του. Μέσα σ’αυτά εντάσσονται και οι θέσεις ενδοωκεάνιας υποβύθισης, που φανερώνουν την διαδικασία έναρξης καταστροφής ωκεάνιου χώρου και συνοδεύονται κυρίως από την δημιουργία μεταμορφικής σόλας.
      Στην παρούσα εργασία, αναφέρονται οι σημαντικές αυτές θέσεις που εντοπίστηκαν και μελετήθηκαν στο Ελληνικό ορογενές, αλλά και οι σημαντικότερες ανάλογες θέσεις στην Αλπική αλυσίδα. Επίσης, αναφέρονται σημεία όπου σήμερα εξελίσσονται ενδοωκεάνιες υποβυθίσεις στην ενεργό παγκόσμια γεωδυναμική, αφού αποτελούν σημαντικά στοιχεία για να κατανοήσουμε αυτές τις διαδικασίες, καθώς οι γεωτεκτονικές διαδκασίες που εξελίσσονται σήμερα, είναι αυτές που επαναλαμβανόμενες στο γεωλογικό παρελθόν έδωσαν την δημιουργία των ήδη διαμορφωμένων ορογενετικών λωρίδων του πλανήτη.

      In the Tethys orogenic system took place one of the most important orogenic processes on the planet, complex and with individual stages, which finally gave rise to the Alpine orogenic belt, structured by a series of mountains. Starting west from the Atlas mountains in N. Africa, the Pyrenees and the Alps in Europe, where it continues splitting into branches in the Apennines in Italy, the Carpathians and Dinarides in the Balkan area, the Pindos mountain range in the main trunk of the Greek area and in all the Greek mountains, passing through Asia in the Taurides in Turkey, in Syria, in Oman, in the Zagros mountains in Iran, ending in the Himalayas and the southern part of China in the east.
      In the effort to study the geotectonic processes that took place in this system, the scientists tried to identify sites that provide important evidence for its evolution. Among them are included the positions of intra-oceanic subduction, which reveal the process of initial destruction of oceanic space and are mainly accompanied by the creation of a metamorphic sole.
      In this study, these important positions identified and studied in the Hellenic orogene, as well as the most important positions in the Alpine chain, are mentioned. Also, intra-ocean subduction processes which are currently developing in the active global geodynamics are described, since they are important elements to understand these processes, as the geotectonic processes that are evolving today are those that repeatedly in the geological past gave rise to the already formed orogenic belts of the planet.

Πλήρες Κείμενο:

PDF

Αναφορές


Ξενόγλωσση Βιβλιογραφία

A.F. Bingel, P6trologie du massif ophiolitique de Pozanti Karsanti (Taurus cilicien, Turquie); Erude de la partie orientale, These 3ieme Cycle, Univ. Louis Pasteur, Strasbourg (1978) 227 pp.

Agard, P., Jolivet, L., Vrielynck, B., Burov, E., & Monie, P. (2007). Plate acceleration: The obduction trigger?. Earth and Planetary Science Letters, 258(3-4), 428-441.

Agard, P., Searle, M. P., Alsop, G. I., & Dubacq, B. (2010). Crustal stacking and expulsion tectonics during continental subduction: P‐T deformation constraints from Oman. Tectonics, 29(5).

Alavi, M., 1994, Tectonic of the Zagros orogenic belt of Iran: New data and interpretations: Tectonophysics, v. 229, p. 211–238, doi: 10.1016/0040-1951(94)90030-2

Alizadeh, E., Arvin, M., Dargahi, S., 2012. Geochemistry and Petrogenesis of Plagiogranites in the Neyriz Ophiolitic Sequence, Iran: Constraints on Their Origin. Journal of Petrology, 12: 1–14 (in Persian)

Allen, P. A. (2007). The Huqf Supergroup of Oman: Basin development and context for Neoproterozoic glaciation. Earth-Science Reviews, 84(3–4), 139–185.

Al-Riyami, K., Robertson, A., Dixon, J., & Xenophontos, C. (2002). Origin and emplacement of the Late Cretaceous Baer–Bassit ophiolite and its

metamorphic sole in NW Syria. Lithos, 65(1-2), 225-260.

Al-Riyami, K., Robertson, A., Dixon, J., & Xenophontos, C. (2002). Origin and emplacement of the Late Cretaceous Baer–Bassit ophiolite and its metamorphic sole in NW Syria. Lithos, 65(1-2), 225-260.

Ambrose, T. K., Wallis, D., Hansen, L. N., Waters, D. J., & Searle, M. P. (2018). Controls on the rheological properties of peridotite at a palaeosubduction interface: A transect across the base of the Oman–UAE ophiolite. Earth and Planetary Science Letters, 491, 193-206.

Ambrose, T. K., Waters, D. J., Searle, M. P., Gopon, P., & Forshaw, J. B. (2021). Burial, accretion, and exhumation of the metamorphic sole of the Oman‐UAE ophiolite. Tectonics, 40(4), e2020TC006392.

Amidi, S.M., Emami, M.H., and Michel, R., 1984, Alkaline character of Eocene volcanism in the middle part of Iran and its geodynamic situation: Geologische Rundschau, v. 73, p. 917–932, doi: 10.1007/BF01820882.

Anders, B.; Reischmann, T.; Poller, U.; Kostopoulos, D. Age and origin of granitic rocks of the eastern Vardar Zone, Greece: New constraints on the evolution of the Internal Hellenides. J. Geol. Soc. Lond. 2005, 162, 857–870.

Babaie, H.A., Babaei, A., Ghazi, A.M., and Arvin, M., 2006, Geochemical, 40Ar/39Ar age, and isotopic data for crustal rocks of the Neyriz ophiolite, Iran: Canadian Journal of Earth Sciences, v. 43, p. 57–70, doi: 10.1139/e05-111.

Barth, M. G., Mason, P. R., Davies, G. R., Dijkstra, A. H., & Drury, M. R. (2003). Geochemistry of the Othris ophiolite, Greece: evidence for refertilization?. Journal of Petrology, 44(10), 1759-1785.

Baumgartner, P.O., Bernoulli, D., 1976. Stratigraphy and radiolarian Fauna in a Late Jurassic–Early Cretaceous section near Achladi (Evia, Eastern Greece). Eclogae Geologicae Helvetiae 69 (3), 601–626

Bechennec, F., Le Metour, J., Rabu, D., Bourdilon-de-Grissac , C., de Wever, P., and Villey, M., 1990, The Hawasina Nappes: Stratigraphy, palaeogeography and structural evolution of a fragment of the south-Tethyan passive continental margin: Geological Society of London Special Publication, v. 49, p. 213–223, doi: 10.1144/ GSL.SP.1992.049.01.14.

Béchennec, F., Tegyey, M., Le Métour, J., Lemière, B., Lescuyer, J. L., Rabu, D., & Milési, J. P. (1991). Igneous rocks in the Hawasina nappes and the Hajar supergroup, Oman mountains: their significance in the birth and evolution of the composite extensional margin of Eastern Tethys. In Ophiolite Genesis and

Evolution of the Oceanic Lithosphere: Proceedings of the Ophiolite Conference, held in Muscat, Oman, 7–18 January 1990 (pp. 593-611). Dordrecht: Springer Netherlands.

Béchennec, F., Le Métour, J., Platel, J. P., & Roger, J. (1993). Geological map of the Sultanate of Oman. Scale 1: 1.000. 000, with explanatory notes. Muscat, Directorate General of Minerals, Oman Ministry of Petroleum and Minerals.

Benioff, H. (1949). Seismic evidence for the fault origin of oceanic deeps. Geological Society of America Bulletin, 60(12), 1837-1856.

Berberian, M., and King, G.C.P., 1981, Towards a paleogeog raphy and tectonic evolution of Iran: Canadian Journal of Earth Sciences, v. 18, p. 210–265, doi: 10.1139/e81-163.

Berberian, F., and Berberian, M., 1981, Tectono-plutonic epi sodes in Iran, in Gupta, H.K., and Delany, F.M., eds., Zagros, Hindukush, Himalaya Geodynamic Evolution: Washington, D.C., American Geophysical Union, p. 5–32.

Berberian, F., Muir, I.D., Pankhurst, R.J., and Berberian, M., 1982, Late Cretaceous and early Miocene Andean type plutonic activity in northern Makran and Central Iran: Journal of the Geological Society of London, v. 139, p. 605–614, doi: 10.1144/gsjgs.139.5.0605.

Bizimis, M., Salters, V. J. M. & Bonatti, E. (2000). Trace and REE content of clinopyroxenes from supra-subduction zone peridotites. Implications for melting and enrichment processes in island arcs. Chemical Geology 165, 67±85

Blendinger, W., van Vliet, A. T., & Hughes Clarke, M. W. (1990). Updoming, rifting and continental margin development during the Late Palaeozoic in northern Oman. Geological Society, London, Special Publications, 49(1), 27-37.

Bloomer, S. H., Stern, R. J., & Smoot, N. C. (1989). Physical volcanology of the submarine Mariana and Volcano Arcs. Bulletin of Volcanology, 51, 210-224.

Blumenthal Μ., Le systeme structural du Taurus sudanatolien, in: Livre h la M6moire du Professeur P. Fallot, Mem. hors ser. Soc. Geol. Fr. Paris 2 (1960-1963) 611- 662.

Bonneau, M., Godfriaux, I., Moulas, Y., Fourcade, E., Masse, J., 1994. Stratigraphie et structure de la bordure orientale de la double fenêtre du Paikon (Macédoine, Grèce). Bull Geol Soc Greece 30, 105–114

Bonev, N.G., Stampfl i, G.M., 2003. New structural and petrologic data on Mesozoic schists in the Rhodope (Bulgaria): Geodynamic implications. Comptes Rendus - Geosci. 335, 691–699. doi:10.1016/S1631-0713(03)00122-6

Bortolotti, V., Chiari, M., Marcucci, M., Marroni, M., Pandolfi, L., Principi, G., & Saccani, E. (2004). Comparison among the Albanian and Greek ophiolites: in search of constraints for the evolution of the Mesozoic Tethys ocean. Ofioliti, 29, 19-35.

Bortolotti, V., Chiari, M., Marroni, M., Pandolfi , L., Principi, G., Saccani, E., 2013. Geodynamic evolution of ophiolites from Albania and Greece (Dinaric-Hellenic belt): One, two, or more oceanic basins? Int. J. Earth Sci. 102, 783–811. doi:10.1007/s00531-012-0835-7

Bouysse, P., Westercamp, D., & Andreieff, P. (1990). 4. THE LESSER ANTILLES ISLAND ARC1. In Proceedings of the Ocean Drilling Program: Scientific results (Vol. 110, p. 29). College Station, TX: Ocean Drilling Program.

Brown, S.A.M., Robertson, A.H.F., 2004. Evidence for Neotethys rooted within the Vardar suture zone from the Voras Massif, northernmost Greece. Tectonophysics 381, 143–173. doi:10.1016/j.tecto.2002.06.001

Brunn J.H., Contribution ~ letude du Pinde septentrional et d'une partie de la Macedoine occidentale, Ann. Geol. Pays Helleniques 7 (1956) 1-358.

Bucher, K., Frey, M., 1994. Petrogenesis of Metamorphic Rocks. Springer, Berlin, Heidelberg, 318 pp.

Celet, P. (1962): Contribution à lʼétude géologique du ParnasseKiona et dʼune partie des régions méridionales de la Grèce continentale. – Ann. Géol. Pays

Helléniques, 13: 446 p., Athens (Univ. Athens)

Celet, P., Ferrière, J. & Wigniolle, E. (1977): Le problème de lʼorigine des blocs exogènes du mélange à éléments ophiolitiques au Sud du Sperchios et dans le massif de lʼOthrys (Grèce). – Bull. Soc. Géol. Fr., 19 (4): 935–942, Paris (Soc. Géol. France).

Celet, P. (1976): À propos du mélange de type “volcano-sédimentaire” de lʼIti (Grèce méridionale). – Bull. Soc. Géol. Fr., 18: 299–307 and Coll. Int. C.N.R.S. Paris, 244: 103–111.

Celet, P., Ferrière, J. & Wigniolle, E. (1977): Le problème de lʼorigine des blocs exogènes du mélange à éléments ophiolitiques au Sud du Sperchios et dans le massif de lʼOthrys (Grèce). – Bull. Soc. Géol. Fr., 19 (4): 935–942, Paris (Soc. Géol. France).

Chauvet, F., Dumont, T., & Basile, C. (2009). Structures and timing of Permian rifting in the central Oman Mountains (Saih Hatat). Tectonophysics, 475(3-4), 563-574.

Coleman, R. G. (1981). Tectonic setting for ophiolite obduction in Oman. Journal of Geophysical Research: Solid Earth, 86(B4), 2497-2508.

Cowan, R. J., Searle, M. P., & Waters, D. J. (2014). Structure of the metamorphic sole to the Oman Ophiolite, Sumeini Window and Wadi Tayyin: implications for ophiolite obduction processes. Geological Society, London, Special Publications, 392(1), 155-175.

Cozzi, A., Rea, G., & Craig, J. (2012). From global geology to hydrocarbon exploration: Ediacaran-Early Cambrian petroleum plays of India, Pakistan and Oman. Geological Society, London, Special Publications, 366(1), 131–162.

Davidson, J., & Wilson, M. (2011). Differentiation and source processes at Mt Pelee and the Quill; active volcanoes in the Lesser Antilles Arc. Journal of Petrology, 52(7-8), 1493-1531.

Danelian, T. & Robertson, A.H.F. (1995): Radiolarian evidence of Middle Jurassic collapse of the Pelagonian carbonate platform (Kallidromon Mountains, Central Greece). – Geol. Soc. Greece, Spec. Publ., 4: 175–180; Proc. 15th Congr. Carpatho-Balcan Geol. Assoc., September 1995, Athens.

Delaune-Mayer Μ., J. Marcoux, J.F. Parrot and A. Poisson, Mode1e d'evolution m6sozofque de la paleomarge tethysienne au niveau des nappes radiolaritiques et ophiolitiques du Taurus lycien, d'Antalaya et du Baer-Bassit, in: Symposium on the Structural History of the Mediterranean Basin, Split, Biju-

Duval and Montadert, ed. (Editions Technip, Paris, 1977) 79-94.

Danelian, T., & Robertson, A. H. (2001). Neotethyan evolution of eastern Greece (Pagondas Mélange, Evia Island) inferred from radiolarian biostratigraphy

and the geochemistry of associated extrusive rocks. Geological Magazine, 138(3), 345-363.

Delaloye, M., & Desmons, J. (1980). Ophiolites and mélange terranes in Iran: a geochronological study and its paleotectonic implications. Tectonophysics, 68(1-2), 83-111.

Dijkstra, A., Drury, M. R. & Vissers, R. L. M. (2001). Structural petrology of plagioclase peridotites in the West Othris Mountains (Greece): melt impregnation in mantle lithosphere. Journal of Petrology 42, 5±24.

Du Toit, A. (1937). Our wandering continents: an hypothesis of continental drifting. (No Title).

Elitok, Ö., & Drüppel, K. (2008). Geochemistry and tectonic significance of metamorphic sole rocks beneath the Beyşehir–Hoyran ophiolite (SW-Turkey). Lithos, 100(1-4), 322-353.

Elliott, T., Plank, T., Zindler, A., White, W., & Bourdon, B. (1997). Element transport from slab to volcanic front at the Mariana arc. Journal of Geophysical Research: Solid Earth, 102(B7), 14991-15019.

Eubanks, T. M. (1993). Variations in the orientation of the Earth. Contributions of space geodesy to geodynamics: Earth dynamics, 24, 1-54.

Farhoudi, G.H., 1978, A comparison of Zagros geology to island-arcs: The Journal of Geology, v. 86, p. 323–334.

Ferrière. J. (1977). Fails nouveaux concernant la zone isopique maliaque (Grèce continentale orientale). VI Colloq. Gèol. Régions égéennes, 197-210.

Ferriere, J. (1982). Paleogeographies et tectoniques superposées dans les Hellenides internes: les massifs de l’ Othrys et du Pelion. Soc. géol. du Nord, 8, 1 – 970

Forbes, G.A., Jansen, H. S.M. & Schreurs, J., 2010. Lexicon of Oman subsurface stratigraphy. Reference guide to the stratigraphy of Oman’s Hydrocarbon basins, GeoArabia, 373 , Special Publication 5 by Gulf Petro Link.

Frank I. Coulson A. E. M. Nairn et al. (eds.), The Ocean Basins and Margins © Plenum Press, New York 1985.

Frisch, W., Dunkl, I., & Kuhlemann, J. (2000). Post-collisional orogen-parallel large-scale extension in the Eastern Alps. Tectonophysics, 327(3-4), 239-265.

Frisch, W., Meschede, M., Blakey, R. C., Frisch, W., Meschede, M., & Blakey, R. (2011). Plate tectonics and mountain building (pp. 149-158). Springer Berlin Heidelberg.

Froitzheim, N., Jahn-Awe, S., Frei, D., Wainwright, A.N., Maas, R., Georgiev, N., Nagel, T.J., Pleuger, J., 2014. Age and composition of meta-ophiolite from the Rhodope Middle Allochthon (Satovcha, Bulgaria): A test for the maximum-allochthony hypothesis of the Hellenides. Tectonics 33, 1477–1500. doi:10.1002/2014TC003526.

Fryer, P. (1996). Evolution of the Mariana convergent plate margin system. Reviews of Geophysics, 34(1), 89-125.

Fryer, P., Ambos, E. L., & Hussong, D. M. (1985). Origin and emplacement of Mariana forearc seamounts. Geology, 13(11), 774-777.

Galeos, A., Pomoni-Papaioannou, F., Tsaila-Monopolis, S., Turnsek, D., Ioakim, C., 1994. Upper Jurassic-Lower Cretaceous molassic-type sedimentation in the western part of the Almopias subzone, Aridhea Loutra unit (northern Greece). Bull Geol Soc Greece 30, 171–184.

Garfunkel, Z., Anderson, C. A., & Schubert, G. (1986). Mantle circulation and the lateral migration of subducted slabs. Journal of Geophysical Research: Solid Earth, 91(B7), 7205-7223.

Garmon, W. T., Allen, C. D., & Groom, K. M. (2017). Geologic and tectonic background of the Lesser Antilles. Landscapes and landforms of the Lesser Antilles, 7-15.

Gartzos, E., 1986. On the Genesis of Cryptocrystalline Magnesite Deposits in the Ultramafic Rocks of Northern Evia (Greece). PhD Thesis ETH Zuerich, Switzerland, 195 pp.

Gartzos, E., Dietrich, V. J., Migiros, G., Serelis, K., & Lymperopoulou, T. (2009). The origin of amphibolites from metamorphic soles beneath the ultramafic ophiolites in Evia and Lesvos (Greece) and their geotectonic implication. Lithos, 108(1-4), 224-242.

Ghazi, A.M., and Hassanipak, A.A., 2000, Petrology and geochemistry of the Shahr-Babak ophiolite, Central Iran, in Dilek, Y., Moores, E.M., Elthon, D., and Nicolas, A., eds., Ophiolites and Oceanic Crust: New insight from fi eld and the Ocean Drilling Program: Geological Society of America Special Paper 349, p. 485–497.

Ghikas, C., Dilek, Y., & Rassios, A. E. (2010). Structure and tectonics of subophiolitic mélanges in the western Hellenides (Greece): implications for ophiolite emplacement tectonics. International Geology Review, 52(4-6), 423-453.

Ghon, G., Rankey, E. C., Baechle, G. T., Schlaich, M., Ali, S. H., Mokhtar, S., & Poppelreiter, M. C. (2018, June). Carbonate reservoir characterisation of an isolated platform integrating sequence stratigraphy and rock physics in Central Luconia. In 80th EAGE Conference and Exhibition 2018 (Vol. 2018, No. 1, pp. 1-5). European Association of Geoscientists & Engineers.

Glennie, K. W. (1974). Geology of the Oman mountains. Verhandelingen van het Koninklink Nederlands Geologisch Mijnbouwkundig Genootchachp, 1, 423.

Gnos, E., & Nicolas, A. (1996). Structural evolution of the northern end of the Oman Ophiolite and enclosed granulites. Tectonophysics, 254(1-2), 111-137.

Gnos, E. (1998). Peak metamorphic conditions of garnet amphibolites beneath the Semail ophiolite: Implications for an inverted pressure gradient. International Geology Review, 40(4), 281-304.

Godfriaux, I., Ricou, L.E., 1991. Th e Paikon, a tectonic window within the Internal Hellenides, Macedonia, Greece. Comptes Rendus - Acad. des Sci. Ser. II 313, 1479–1484.

Greene, H. G., Collot, J. Y., Fisher, M. A., & Crawford, A. J. (1994). Neogene tectonic evolution of the New Hebrides island arc: A review incorporating ODP drilling results. In Proceedings of the Ocean Drilling Program, Scientific Results (Vol. 134, No. 1, pp. 19-46). College Station, TX: Ocean Drilling Program.

Guilmette, C., Smit, M. A., van Hinsbergen, D. J., Gürer, D., Corfu, F., Charette, B., ... & Savard, D. (2018). Forced subduction initiation recorded in the sole and crust of the Semail Ophiolite of Oman. Nature Geoscience, 11(9), 688-695.

Hacker, B. R., Mosenfelder, J. L., & Gnos, E. (1996). Rapid emplacement of the Oman ophiolite: Thermal and geochronologic constraints. Tectonics, 15(6), 1230-1247.

Hallas, P., & Bauer, W. (2021). Texture and Shape Analysis of Quartzite Mylonites of the Metamorphic Sole of the Samail Ophiolite (Oman): Evidence for Syn-and Post-Obduction Deformation. Geosciences, 11(3), 111.

Hassanipak, A. A., & Ghazi, A. M. (2000). Petrology, geochemistry and tectonic setting of the Khoy ophiolite, northwest Iran: implications for Tethyan tectonics. Journal of Asian Earth Sciences, 18(1), 109-121.

Hatzipanagiotou, K., Tsikouras, B., Migiros, G., Gartzos, E., Serelis, K., 2003. Origin of rodingites in ultramafic rocks from Lesvos island (NE Aegean, Greece). Ofioliti 28 (1), 13–23.

Hynes, A. (1974). Igneous activity at the birth of an ocean basin in eastern Greece. Canadian Journal of Earth Sciences 11, 842±853.

Jahn-Awe, S., Froitzheim, N., Nagel, T.J., Frei, D., Georgiev, N., Pleuger, J., 2010. Structural and geochronological evidence for Paleogene thrusting in the

western Rhodopes, SW Bulgaria: Elements for a new tectonic model of the Rhodope Metamorphic Province. Tectonics 29, 1–30. doi:10.1029/2009TC002558

Jones, G. and Robertson, A.H.F. (1991). Tectono-stratigraphy and evolution of the Mesozoic Pindos ophiolite and related units, northwestern Greece. Journ. Geol. Soc. London, vol.148, pp.267-288.

Juteau T., Ophiolites des Taurides: essai sur leur histoire oceanique, Rev. Geol. Dyn. Geogr. Phys. 21, 3 (1979) 191-214.

Juteau T., Les ophiolites des nappes d'Antalaya (Taurides occidentales, Turquie), Petrologie d'un fragment de l'ancienne crofite oceanique tethysienne, Sciences de la Terre, Nancy, Mem. 32 (1975) 692 pp.

Juteau, T. (1980). Ophiolites of Turkey.

Karipi, S. (2004): The ophiolitic outcrops of Iti and Kallidromon. Geological study – petrogenetic evolution – geotectonic interpretation. – Ph. D. thesis Univ. Patras: 417 p., Patras.

Katrivanos, E., Kilias, A., Mountrakis, D., 2013. Kinematics of deformation and structural evolution of the Paikon Massif (Central Macedonia, Greece): A Pelagonian tectonic window? Neues Jahrb. für Geol. und Paläontologie - Abhandlungen 269, 149–171. doi:10.1127/0077- 7749/2013/0342.

Kazmin, V.G., Kulakov, V.V., 1968. The geological map of Syria. Scale 1:50,000 (Sheet Al-Latheqiyeh). Explanatory note. Technoexport, Nedra, Moscow, 124 pp.

Katsikatsos, G., 1977. La structure téctonique d'Attique et de l'Ile d'Eubée.VI Colloquium on the Geology of the Aegean Region. Athens I, 211–228.

Katsikatsos, G., Mataragas, D., Migiros, G., Triandaphyllidis, E., 1982. Geological study of Lesvos island. I.G.M.E. report. 92 pp.

Katsikatsos, G., Migiros, G., Triandaphyllidis, E., Mettos, A., 1986. Geological structure of the Internal Hellenides (E. Thessaly–Euboea–Attica–Northern Cyclades and Lesvos). Geological and Geophysical Research. I.G.M.E., pp. 191–212. special issue.

Katsikatsos, G., Migiros, G., Triantaphyllis, M. and Mettos, A. (1986). Geological structure of the internal Hellenides (E. Thessaly - SW. Macedonia, Euboea - Attica - Northern Cyclades Islands and Lesvos). I.G.M.E. Geological and Geophysical Research, Sp.Issue, pp.191-212

Kilias, A., Mountrakis, D., 1998. Tertiary extension of the Rhodope massif associated with granite emplacement (Northern Greece). Acta Vulcanol. 10, 331–337.

Kilias, A., Frisch, W., Avgerinas, A., Dunkl, I., Falalakis, G., Gawlick, H.-J., 2010. Alpine architecture and kinematics of deformation of the northern Pelagonian nappe pile in the Hellenides. Austrian J. Earth Sci. 103, 4–28

Kilias, A.; Thomaidou, E.; Katrivanos, E.; Vamvaka, A.; Fassoulas, C.; Pipera, K.; Falalakis, G.; Avgerinas, S.; Sfeikos, A. A geological cross-section through northern Greece from Pindos to Rhodope Mountain Ranges: A field guide accross the Ex-ternal and Internal Hellenides. J. Virtual Explor. 2016, 50, 1–107.

Kilias, A. The Alpine Geological History of the Hellenides from the Triassic to the Present—Compression vs. Extension, a Dynamic Pair for Orogen Structural Configuration: A Synthesis. Geosciences 2024, 14, 10. https://doi.org/ 10.3390/geosciences14010010

Koroneos, A., Kilias, A., Avgerinas, A., 2013. Hercynian plutonic rocks of Voras Mountain, Macedonia, Northern Greece: their structure, petrogenesis, and tectonic signifi cance. Int. Geol. Rev. 55, 994–1016. doi:10.1080/0020681 4.2012.758830.

Leat, P. T., & Larter, R. D. (2003). Intra-oceanic subduction systems: introduction. Geological Society, London, Special Publications, 219(1), 1-17.

Leluc, H. (1978): Contribution à lʼétude géologique du Massif du Kallidromon (Grèce continentale). – Diplôme dʼÉtudes Approfondies Univ. Lille: 74 p., Lille.

L.E. Ricou, I. Argyriadis and J. Marcoux, L'axe caicaire du Taurus, un alignement de fenetres arabo-africaines sous des nappes radiolaritiques, ophiolitiques et metamorphiques, Bull. Soc. Geol. Fr. 17, 6 (1975) 1024- 1043.

Makris, J. (1985). Geophysics and geodynamic implications for the evolution of the Hellenides. In Geological evolution of the Mediterranean Basin:

Raimondo Selli commemorative volume (pp. 231-248). New York, NY: Springer New York.

Mann, P., Taylor, F. W., Lagoe, M. B., Quarles, A., & Burr, G. (1998). Accelerating late Quaternary uplift of the New Georgia Island Group (Solomon island arc) in response to subduction of the recently active Woodlark spreading center and Coleman seamount. Tectonophysics, 295(3-4), 259-306.

Massonne, H. J., Opitz, J., Theye, T., & Nasir, S. (2013). Evolution of a very deeply subducted metasediment from As Sifah, northeastern coast of Oman. Lithos, 156, 171-185.

McKenzie, D. P. (1969). Speculations on the consequences and causes of plate motions. Geophysical Journal International, 18(1), 1-32.

Meinhold, G., Kostopoulos, D., Reischmann, T., Frei, D., BouDagher-Fadel, M.K., 2009. Geochemistry, provenance and stratigraphic age of metasedimentary rocks from the eastern Vardar suture zone, northern Greece. Palaeogeogr. Palaeoclimatol. Palaeoecol. 277, 199–225. doi:10.1016/j.palaeo.2009.04.005

Menzies, M. (1973). Mineralogy and partial melt textures within an ultramafic±mafic body, Greece. Contributions to Mineralogy and Petrology 42, 273±285.

Menzies, M. & Allen, C. (1974). Plagioclase lherzolite±residual mantle relationships within two eastern Mediterranean ophiolites. Contributions to Mineralogy and Petrology 45, 197±213.

Menzies, M. (1976). Rare earth geochemistry of fused ophiolitic and alpine lherzolitesÐI. Othris, Lanzo and Troodos. Geochimica et Cosmochimica Acta 40, 645±656.

Mercier, J. Étude géologique des zones internes des Hellénides en Macédoine centrale (Grèce). Contribution é l’ étude du métamorphisme et de l’ évolution magmatique des zones internes des Hellénides. Ann. Géol. Pays Helléniques 1968, 20, 1–792.

Michail, M., Pipera, K., Koroneos, A., Kilias, A., Ntaflos, T., 2016. New perspectives on the origin and emplacement of the Late Jurassic Fanos granite, associated with an intra-oceanic subduction within the Neotethyan Axios-Vardar Ocean. Int. J. Earth Sci. 105, 1965–1983. doi:10.1007/s00531-016-1321-4

Michail, M.; Pipera, K.; Koroneos, A.; Kilias, A.; Ntaflos, T. New perspectives on the origin and emplacement of the Late Jurassic Fanos granite, associated with an intra-oceanic subduction within the Neotethyan Axios-Vardar Ocean. Int. J. Earth Sci. 2016, 105, 1965–1983.

Migiros, G., Hatzipanagiotou, K., Gatzos, E., Serelis, K., Tsikouras, B., 2000. Petrogenetic evolution of ultramafic rocks from Lesvos island (NE Aegean, Greece). Chemie der Erde 60, 27–46.

Mohajjel, M., Fergusson, C.L., and Sahandi, M.R., 2003, Cretaceous-Tertiary convergence and continental collision, Sanandaj-Sirjan zone, western Iran: Journal of Asian Earth Sciences, v. 21, p. 397–412, doi: 10.1016/ S1367-9120(02)00035-4

Moores, E. M. (1982). Origin and emplacement of ophiolites. Reviews of Geophysics, 20(4), 735-760.

Moghadam, H. S., Stern, R. J., & Rahgoshay, M. (2010). The Dehshir ophiolite (central Iran): Geochemical constraints on the origin and evolution of the Inner Zagros ophiolite belt. Bulletin, 122(9-10), 1516-1547.

Moghadam, H. S., Whitechurch, H., Rahgoshay, M., & Monsef, I. (2009). Significance of Nain-Baft ophiolitic belt (Iran): Short-lived, transtensional Cretaceous back-arc oceanic basins over the Tethyan subduction zone. Comptes Rendus Geoscience, 341(12), 1016-1028

Mountrakis, D., Sapountzis, E., Kilias, A., Eleftheriadis, G., & Christofides, G. (1983). Paleogeographic conditions in the western Pelagonian margin in Greece during the initial rifting of the continental area. Canadian Journal of Earth Sciences, 20(11), 1673-1681.

Mountrakis, D.M., 1986. Th e Pelagonian Zone in Greece: A Polyphase-Deformed Fragment of the Cimmerian Continent and Its Role in the Geotectonic Evolution of the Eastern Mediterranean. J. Geol. 94, 335–34

Mountrakis, D., Kilias, Α., Zouros, N. (1993). Kinematic analysis and Tertiary evolution of the Pindos-Vourinos ophiolites (Epirus-Western Macedonia, Greece). Bull. Geol. Soc. Greece, 28, 111-124.

Nakanishi, M., Tamaki, K., & Kobayashi, K. (1989). Mesozoic magnetic anomaly lineations and seafloor spreading history of the northwestern Pacific. Journal of Geophysical research: solid earth, 94(B11), 15437-15462.

Nicolas, A., Boudier, F., & Ildefonse, B. (1996). Variable crustal thickness in the Oman ophiolite: Implication for oceanic crust. Journal of Geophysical Research: Solid Earth, 101(B8), 17941-17950.

Nicolas, A., Boudier, F., Ildefonse, B., & Ball, E. (2000). Accretion of Oman and United Arab Emirates ophiolite–Discussion of a new structural map. Marine Geophysical Researches, 21, 147-180.

Ninkabou, D., Agard, P., Nielsen, C., Smit, J., Gorini, C., Rodriguez, M., ... & Ducassou, C. (2021). Structure of the offshore obducted Oman margin: Emplacement of Semail ophiolite and role of tectonic inheritance. Journal of Geophysical Research: Solid Earth, 126(2), 2020JB020187.

Nirta, G., Bortolotti, V., Chiari, M., Menna, F., Saccani, E., Principi, G., & Vannucchi, P. (2010). Ophiolites from the Grammos-Arrenes area, northern Greece: geological, paleontological and geochemical data. Ofioliti, 35, 103-115.

Ozsvárt, P., & Kovács, S. (2012). Revised Middle and Late Triassic radiolarian ages for ophiolite mélanges: implications for the geodynamic evolution of the northern part of the early Mesozoic Neotethyan subbasins. Bulletin de la Société géologique de France, 183(4), 273-286.

Papanikolaou, D.J., 1996. The tectonostratigraphic terranes of the Hellenides. In: Papanikolaou, D., Sassi, F.P. (Eds.), IGCP Project No. 276, Terrane Maps and Terrane Descriptions. Annales Géologie des Pays Helléniques 37, 1996–1977, pp. 495–514.

Papanikolaou, D. (1999). The Triassic ophiolites of Lesvos Island within the Cimmeride orogene event. EUG 10, Symposium D06: Inter-Relations between

Palaeotethys and Neotethys in Europe and Asia, p.315.

Papastamatiou, J., Tataris, A., Vetoulis, D., Katsikatsos, G., Lalechos, N. & Elefteriou, A. (1962a): Geological map of Amfi klia 1 : 50 000, Inst. Geol. Subsurface Research (I.G.S.R.).

Papastamatiou, J., Vetoulis, D. & Tataris, A. (1962b): Kallidromon. Géologie et correlation avec le Parnasse. – Ann. Géol. Pays Helléniques, 5 (1): 43–51, Athens (Univ. Athens).

Papastamatiou, J., Tataris, A., Vetoulis, D., Bornovas, J., Katsikatsos, G., Maragoudakis, N. & Lalechos, N. (1967): Geological map of Lamia 1 : 50 000, Inst. Geol. Subsurface Research (I.G.S.R.).

Papastamatiou, J., Tataris, A., Vetoulis, D., Bornovas, J., Christodoulou, G. & Katsikatsos, G. (1960): Geological map of Amfissa 1 : 50 000, Inst. Geol. Subsurface Research (I.G.S.R.).

Parlak, O., & Delaloye, M. (1996). Geochemistry and timing of post‐metamorphic dyke emplacement in the Mersin Ophiolite (southern Turkey): New age constraints from 40Ar/39Ar geochronology. Terra Nova, 8(6), 585-592.

Parlak, O., & Delaloye, M. (1999). Precise 40Ar/39Ar ages from the metamorphic sole of the Mersin ophiolite (southern Turkey). Tectonophysics, 301(1-2), 145-158.

Parrot J.F., Le cortege ophiolitique du Pinde septentrional, Grece, These 3i~me Cycle, ORSTOM (1967) 114 pp.

Parrot, J.F., Guernet, C., 1972. Le cortège ophiolitique de l'Eubèe mozonne, (Grèce): étude pétrographique des formations volcaniques et des roches métamorphiques associées dans les Monts Kandili aux radiolarites. Cahier ORSTOM, Serie Géologiques, vol. 4, pp. 153–163

Parrot, J.F., 1974a. Le Secteur de Tamima (Turkmannli): Etude d’ une sequence volcano-sedimentaire de la region ophiolitique du Baer –Bassit (Nord-Ouest de la Syrie). Cah.-ORSTOM, Ser. Geol. VI (2), 127 – 146.

Parrot, J.F., 1974b. L’assemblage ophiolitique du Baer – Bassit (Nord-Ouest de la Syrie): e´tude pe´trographique et ge´ochimique du complexe filonien des laves en coussins qui lui sont associe´es, et d’une partie des formations effusives du volcano-se´dimentaire. Cah.-ORSTOM, Se´r. Ge´ol. VI (2), 94 – 126.

Parrot, J.F., 1980. The Baer –Bassit (Northwestern Syria) ophiolitic area. Ofioliti 2, 279 – 295.

P.C. De Graciansky, Recherches gdologiques dans le Taurus Lycien, These Univ. Paris XI. Orsay, Sr. A, 896 (1972) 571 pp.

Pearce, J. A., Lippard, S. J. & Roberts, S. (1984). Characteristics and tectonic significance of supra-subduction zone ophiolites. In: Kokelaar, P. B. & Howells, M. F. (eds) Marginal Basin Geology. Geological Society, London, Special Publications 16, 77±94

Petterson, M. G., & Tawake, A. K. (2016). Toward inclusive development of the Pacific region using geoscience. Geoscience for the public good and global development: toward a sustainable future. Geological Society of America Special Paper, 520, 459-478.

Polat, A., Casey J.F., Kerrich, R. (1996). Geochemical characteristics of accreted material beneath the Pozanti-Karsanti ophiolite, Turkey: Intra-oceanic detachment, assembly and obduction. Tectonophysics, 249-276.

Rabu, D., Le Métour, J., Béchennec, F., Beurrier, M., Villey, M., & Bourdillon-Jeudy De Grissac, C. (1990). Sedimentary aspects of the Eo-Alpine cycle on the northeast edge of the Arabian Platform (Oman Mountains). Geological Society, London, Special Publications, 49(1), 49-68.

Rassios, A. & Konstantopoulou, G. (1993). Emplacement tectonism and the position of chrome ores in the Mega Isoma peridotites, SW Othris, Greece. Bulletin of the Geological Society of Greece 28, 463±474

Rassios, A. & Smith, A. G. (2001). Constraints on the formation and emplacement age of western Greek ophiolites (Vourinos, Pindos, and Othris) inferred from deformation structures in peridotites. In: Dilek, Y., Moores, E., Elthon, D. & Nicolas, A. (eds) Ophiolites and Oceanic Crust: New Insights from Field

Studies and the Ocean Drilling Program. Geological Society of America, Special Papers 349, 473±484.

Rassios, A. H., & Moores, E. M. (2006). Heterogeneous mantle complex, crustal processes, and obduction kinematics in a unified Pindos-Vourinos ophiolitic slab (northern Greece). Geological Society, London, Special Publications, 260(1), 237-266

Rassios, A. E., & Dilek, Y. (2009). Rotational deformation in the Jurassic Mesohellenic ophiolites, Greece, and its tectonic significance. Lithos, 108(1-4), 207-223.

Ricou, L.E., 1971, Le croissant ophiolitique peri-Arabe une ceinture de nappes mise en place au cretace superieur: Revue de Géographie Physique et de Géologie Dynamique, v. 13, p. 327–350.

Ricou, L.E., 1974, L’Étude Géologique de la Région de Neyriz (Zagros Iranien) et l’Évolution Structurale des Zagrides [Thèse d’Etat]: Orsay, Paris-Sud, 300 p.

Ricou, L.E., 1976, Evolution Structurale des Zagrides. La Région Clef de Neyriz (Zagros Iranien): Memoire Societé Geologie de la France 125, 140 p.

(Thèse Orsay, 1974).

Ricou, L.E., Braud, J., and Brunn, J.H., 1977, Le Zagros: Memoire Societé Geologie de la France 8, p. 33–52.

Richter, D., Müller, C. & Mihm, A. (1993): Die Flysch-Zonen Griechenlands, V. Zur Stratigraphie des Flysches der PindosZone im nördlichen Pindos-Gebirge

zwischen der albanischen Grenze und der Querzone von Kastanitikos (Griechenland). – N. Jb. Geol. Paläont. Mh., 5: 257–291, Stuttgart (Schweizerbart)

Ricou, L.E., Burg, J.P., Godfriaux, I., Ivanov, Z., 1998. Rhodope and Vardar: Th e metamorphic and the olistostromic paired belts related to the Cretaceous subduction under Europe. Geodin. Acta 11, 285–309. doi:10.1016/S0985- 3111(99)80018-7

Rioux, M., Garber, J., Bauer, A., Bowring, S., Searle, M., Kelemen, P., & Hacker, B. (2016). Synchronous formation of the metamorphic sole and igneous crust of the Semail ophiolite: New constraints on the tectonic evolution during ophiolite formation from high-precision U–Pb zircon geochronology. Earth and

Planetary Science Letters, 451, 185-195.

Robertson, A.H.F., 2002. Overview of the genesis and emplacement of Mesozoic ophiolites in the Eastern Mediterranean Tethyan region. Lithos 65, 1–67.

Sabzehei, M., 1997, The Geological Map of Dehshir, 1:100,000 Series: Tehran, Iran, Geological Survey of Iran, Sheet 6752, scale 1:100,000.

Saccani, E., & Photiades, A. (2004). Mid-ocean ridge and supra-subduction affinities in the Pindos ophiolites (Greece): implications for magma genesis in a forearc setting. Lithos, 73(3-4), 229-253.

Saccani, E., Bortolotti, V., Marroni, M., Pandolfi , L., Photiades, A., Principi, G., 2008. Th e Jurassic association of backarc basin ophiolites and calc-alkaline volcanics in the Guevgueli complex (northern Greece): Implication for the evolution of the Vardar zone. Ofioliti 33, 209–227

Schenker, F.L., Burg, J.P., Kostopoulos, D., Moulas, E., Larionov, A., Von Quadt, A., 2014. From mesoproterozoic magmatism to collisional cretaceous anatexis: Tectonomagmatic history of the Pelagonian Zone, Greece. Tectonics 33, 1552–1576. doi:10.1002/2014TC003563

Schmid, S.M., Bernoulli, D., Fügenschuh, B., Maenco, L., Schefer, S., Schuster, R., Tischler, M., Ustaszewski, K., 2008. Th e Alpine-Carpathian-Dinaridic orogenic system: Correlation and evolution of tectonic units. Swiss J. Geosci. 101, 139–183. doi:10.1007/s00015-008-1247-3

Schuth, S., Münker, C., König, S., Qopoto, C., Basi, S., Garbe-Schönberg, D., & Ballhaus, C. (2009). Petrogenesis of lavas along the Solomon Island Arc,

SW Pacific: Coupling of compositional variations and subduction zone geometry. Journal of Petrology, 50(5), 781-811.

Searle, M. P., & Malpas, J. (1980). Structure and metamorphism of rocks beneath the Semail ophiolite of Oman and their significance in ophiolite obduction. Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 71(4), 247-262.

Searle, M. P., & Malpas, J. (1982). Petrochemistry and origin of sub-ophiolitic metamorphic and related rocks in the Oman Mountains. Journal of the geological society, 139(3), 235-248.

Searle, M. P., & Cox, J. O. N. (2002). Subduction zone metamorphism during formation and emplacement of the Semail ophiolite in the Oman Mountains. Geological Magazine, 139(3), 241-255.

Searle, M.P. Structural geometry, style and timing of deformation in the Hawasina Window, Al Jabal al Akhdar and Saih Hatat culminations, Oman Mountains. GeoArabia 2007, 12, 99–130.

Searle, M. P., Cherry, A. G., Ali, M. Y., & Cooper, D. J. (2014). Tectonics of the Musandam Peninsula and northern Oman Mountains: From ophiolite obduction to continental collision. GeoArabia, 19(2), 135-174.

Searle, M. P., Waters, D. J., Garber, J. M., Rioux, M., Cherry, A. G., & Ambrose, T. K. (2015). Structure and metamorphism beneath the obducting Oman ophiolite: Evidence from the Bani Hamid granulites, northern Oman mountains. Geosphere, 11(6), 1812-1836.

Searle, M., Rioux, M., & Garber, J. M. (2022). One line on the map: a review of the geological history of the Semail Thrust, Oman-UAE mountains. Journal of Structural Geology, 158, 104594.

Şenel, M., 1984. Discussion on the Antalya nappes. In: Tekeli, O., Göncüoğlu, M.C. (Eds.), Geology of the Taurus Belt, Proceedings of the International Symposium. Mineral Research and Exploration Institute of Turkey (MTA) Ankara, Turkey, pp. 41.

Serelis, K.G., 1995. Investigation of the Ophiolites of Lesvos Island. PhD Thesis Agricultural University Athens, 241 pp.

Shafaii Moghadam, H., Stern, R. J., Chiaradia, M., et al., 2013. Geochemistry and Tectonic Evolution of the Late Cretaceous Gogher-Baft Ophiolite, Central Iran. Lithos, 168– 169: 33–47. doi:10.1016/j.lithos.2013.01.013.

Shahabpour, J., 2007, Island-arc affi nity of the Central Iranian volcanic belt: Journal of Asian Earth Sciences, v. 30, p. 652–665, doi: 10.1016/j.jseaes.2007.02.004.

Sharp, I.R., Robertson, a. H.F., 2006. Tectonic-sedimentary evolution of the western margin of the Mesozoic Vardar Ocean: evidence from the Pelagonian and Almopias zones, northern Greece. Geol. Soc. London, Spec. Publ. 260, 373–412. doi:10.1144/GSL.SP.2006.260.01.16

Simantov, J., Economou, C., Bertrand, J., 1990. Metamorphic rocks associated with the Central Euboea ophiolite (Southern Greece): some new occurrences. In: Malpas, J., Moores, E.M., Panayiotou, A., Xenophontos, C. (Eds.), Oceanic Crust Analogues. Proceedings of the Symposium “Troodos 1987”. Geological Survey Department, Ministry of Agriculture and Natural Resources, Nicosia, Cyprus, pp. 285–293.

Smith, A. G., Hynes, A. J., Menzies, M., Nisbet, E. G., Price, I., Welland, M. J. & Ferriere, J. (1975). The stratigraphy of the Othris Mountains, eastern central Greece: a deformed Mesozoic continental margin sequence. Eclogae Geologicae Helveticae 68, 463±481.

Smith, A. G. (1993). Tectonic significance of the Hellenic±Dinaric ophiolites. In: Prichard, H. M., Alabaster, T., Harris, N. B. W. & Neary, C. R. (eds) Magmatic Processes and Plate Tectonics. Geological Society, London, Special Publications 76, 213±243

Smith, I. E., Stewart, R. B., & Price, R. C. (2003). The petrology of a large intra-oceanic silicic eruption: the Sandy Bay Tephra, Kermadec Arc, Southwest Pacific. Journal of Volcanology and Geothermal Research, 124(3-4), 173-194.

Smith, I. E., & Price, R. C. (2006). The Tonga–Kermadec arc and Havre–Lau back-arc system: their role in the development of tectonic and magmatic models for the western Pacific. Journal of volcanology and geothermal research, 156(3-4), 315-331.

Smith, I. E., Stewart, R. B., Price, R. C., & Worthington, T. J. (2010). Are arc-type rocks the products of magma crystallisation? Observations from a simple oceanic arc volcano: Raoul Island, Kermadec Arc, SW Pacific. Journal of Volcanology and Geothermal Research, 190(1-2), 219-234

Soret, M., Agard, P., Dubacq, B., Plunder, A., & Yamato, P. (2017). Petrological evidence for stepwise accretion of metamorphic soles during subduction infancy (Semail ophiolite, Oman and UAE). Journal of Metamorphic Geology, 35(9), 1051-1080.

Soret, M., Agard, P., Ildefonse, B., Dubacq, B., Prigent, C., & Rosenberg, C. (2019). Deformation mechanisms in mafic amphibolites and granulites: Record from the Semail metamorphic sole during subduction infancy. Solid Earth, 10(5), 1733-1755.

Stampfli, G.M. (1996): The intra-Alpine terrain: a Paleotethyan remnant in the Alpine Variscides. – Eclogae Geol. Helv., 89 (1): 13–42, Basel (Birkhäuser).

Stampfl i, G.M., Mosar, J., De Bono, A. & Vavassis, I. (1998): Late Paleozoic, Early Mesozoic plate tectonics of the western Tethys. – 8th Int. Congr. Geol.

Soc. Greece, Patras, Greece, 32 (1): 113– 120, Patras.

Stern, R. J., Reagan, M., Ishizuka, O., Ohara, Y., & Whattam, S. (2012). To understand subduction initiation, study forearc crust: To understand forearc crust, study ophiolites. Lithosphere, 4(6), 469-483.

Spray, J.G. and Roddick, J.C. (1980). Petrology and 40Ar/39Ar geochronology of some Hellenic sub-ophiolite metamorphic rocks. Contrib. Mineral. Petrol., 72, 43-55.

Stocklin, J., 1977, Structural correlation of the Alpine range between Iran and Central Asia: Societé Geologie de la France Memoire Hors-Serve 8, p. 333–353.

Sun, C. H., & Stern, R. J. (2001). Genesis of Mariana shoshonites: Contribution of the subduction component. Journal of Geophysical Research: Solid Earth, 106(B1), 589-608.

Tamura, Y., & Tatsumi, Y. (2002). Remelting of an andesitic crust as a possible origin for rhyolitic magma in oceanic arcs: an example from the Izu–Bonin arc. Journal of Petrology, 43(6), 1029-1047.

Tamura, Y., Busby, C. J., Blum, P., Guèrin, G., Andrews, G. D. M., Barker, A. K., ... & Yang, Y. (2015). Expedition 350 summary. In Proceedings of the International Ocean Discovery Program (Vol. 350).

Tavani, S., Corradetti, A., Sabbatino, M., Seers, T. & Mazzoli, S., 2020. Geological record of the transition from induced to self-sustained subduction in the Oman Mountains, J. Geodyn., 133, doi:10.1016/j.jog.2019.101674.

Taylor, B. (1992). Island arcs, deep-sea trenches, and back-arc basins. Oceanus, 35(4), 17-26.

Taylor, F. W., Bevis, M. G., Schutz, B. E., Kuang, D., Recy, J., Calmant, S., ... & Reichenfeld, C. (1995). Geodetic measurements of convergence at the New Hebrides island arc indicate arc fragmentation caused by an impinging aseismic ridge. Geology, 23(11), 1011-1014.

Taylor, R. N., & Nesbitt, R. W. (1998). Isotopic characteristics of subduction fluids in an intra-oceanic setting, Izu–Bonin Arc, Japan. Earth and Planetary Science Letters, 164(1-2), 79-98.

Terry J., Ensembles lithologiques et structures internes du cortege ophiolitique du Pinde septentrional (Grace), Construction d'un modele petrogenetique, Bull. Soc. Geol. Fr. 21 (1974) 204-213.

Terry J. and J. Mercier, Sur l'existence d'une serie d6tritique berriasienne intercal6e entre la nappe des ophiolites 310 et le flysch 6oc~ne de la nappe du Pinde (Pinde septentrional, Grace), C.R. Somm. Soc. Geol. Fr. 2 (1971) 71- 73.

Thomas, R. J., Ellison, R. A., Goodenough, K. M., Roberts, N. M., & Allen, P. A. (2015). Salt domes of the UAE and Oman: probing eastern Arabia. Precambrian Research, 256, 1-16.

Thuizat, R., Whitechurch, H., Montigny, R., and Juteau, T. (1981). K-Ar Dating of some Inra-Ophiolitic metamorphic soles from the eastern Mediterranean: new evidence for oceanic thrustings before obduction. Earth and Planetary Science Letters, 52, 302-310.

Tsikouras, B., Pomonis, P., & Hatzipanagiotou, K. (2008). Geological evolution of the Iti and Kallidromon Mountains (central Greece), focused on the ophiolitic outcrops.

U. Cakir, T. Juteau and H. Whitechurch, Nouvelles preuves de l'ecaillage intra-oc6anique precoce des ophiolltes tethysiennes: les roches m6tamorphiques infraperidotitiques du massif de Pozanti-Karsanti (Turquie), Bull. Soc. Geol. Fr. 20, I (1978) 61-70.

U. Cakir, Petrologie du massif ophiolitique de Pozanti Karsanti (Taurus Cilicien, Turquie); Etude de la partie cantrale, These Doct. Ingenieur, Univ. Louis Pasteur, Strasbourg (1978) 251 pp.

Vergely, P. Tectoniques des Ophiolites Dans les Hellénides Internes Déformation, Métamorphisme et Phénomènes Sédi-Mentaires. Conséquences sur l’ Évolution des Région Téthysiennes Occidentales. Ph.D. Thesis, University Paris-Sud, Orsay, Paris, France, 1984; pp. 1–560.

Von Huene, R., & Scholl, D. W. (1991). Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust. Reviews of Geophysics, 29(3), 279-316.

Wegener, A. (1966). The origin of continents and oceans. Courier Corporation.

Weidle, C., Wiesenberg, L., El-Sharkawy, A., Krüger, F., Scharf, A., Agard, P., & Meier, T. (2022). A 3-D crustal shear wave velocity model and Moho map below the Semail Ophiolite, eastern Arabia. Geophysical Journal International, 231(2), 817-834.

Whitehouse, M. J., Pease, V., & Al-Khirbash, S. (2016). Neoproterozoic crustal growth at the margin of the East Gondwana continent–age and isotopic constraints from the easternmost inliers of Oman. International Geology Review, 58(16), 2046-2064.

Wigniolle, E. (1977a): Contribution à lʼétude géologique du massif de lʼIti (Grèce continentale). – Thèse 3e cycle Univ. Lille: 239 p., Lille.

Wigniolle, E. (1977b): Données nouvelles sur la géologie du massif de lʼIti (Grèce continentale). – Ann. Soc. Géol. Nord, 47 (3): 239–251, Villeneuve dʼAscq.

Wilson, J. T. (1973). Mantle plumes and plate motions. Tectonophysics, 19(2), 149-164.

Wilson, M. (Ed.). (1989). Igneous petrogenesis. Dordrecht: Springer Netherlands.

Yamato, P., Agard, P., Goffé, B., De Andrade, V., Vidal, O., & Jolivet, L. (2007). New, high-precision P–T estimates for Oman blueschists: Implications for obduction, nappe stacking and exhumation processes. Journal of Metamorphic Geology, 25(6), 657–682.

Ελληνική Βιβλιογραφία

Διανέλλου, Η., 2020. Η γεωχημεία των μαγμάτων που δημιουργούνται στα διαφορετικά είδη νησιωτικών τόξων. Διπλωματική Ερργασία, Τμήμα Γεωλογίας Α.Π.Θ.

Θωμαΐδου, Ε. (2009). Η Γεωλογική δομή της Νήσου Λέσβου. Διδακτορική διατριβή, Τμήμα Γεωλογίας, Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης, 200 σελ.

Κατσικάτσος, Γ., Ματαράγκας, Δ., Μιγκίρος, Γ. και Τριανταφύλλης Μ. (1982). Γεωλογική μελέτη της Νήσου Λέσβου. Ι.Γ.Μ.Ε., Αθήνα, σελ.90, (1991).

Μουντράκης, Δ. (1994). Εισαγωγή στη γεωλογία της Μακεδονίας και της Θράκης. Απόψεις για τη γεωτεκτονική εξέλιξη της ελληνικής ενδοχώρας και των εσωτερικών ελληνίδων. Δελτ. Ελ. Γεωλ. Ετ. 30/1, 31-46.

Μουντράκης, Δ., 2010. Γεωλογία Ελλάδος. Εκδόσεις UNIVERSITY STUDIO PRESS, Θεσσαλονίκη.

Παπαζάχος Β., Παπαζάχος Κ., 2008. Εισαγωγή στη γεωφυσική. Εκδόσεις Ζήτη, Νοέμβριος 2008.

Διαδικτυακές Πηγές

https://oceanexplorer.noaa.gov/okeanos/explorations/ex1605/background/geology/welcome.html

https://earth.google.com/web/@48.59671297,54.94602217,282.61778042a,11758957.37067819d,35y,-0h,0t,0r/data=OgMKATA


Εισερχόμενη Αναφορά

  • Δεν υπάρχουν προς το παρόν εισερχόμενες αναφορές.