FAULTING DEFORMATION OF THE MESOHELLENIC TROUGH IN THE KASTORIA-NESTORION REGION (WESTERN MACEDONIA, GREECE)
Περίληψη
The Kastoria-Nestorion region, which belongs to the Tertiary MesoHellenic Trough (MHT), is a low relief NW-SE trending intermountainous basin filled with Tertiary molasse-type sedimentary rocks and nowadays drained by the Aliakmnonas River and its tributaries. In the present work, the large fault zones in the region and the general fault pattern are defined, mapped and described with the aid of satellite images. In addition, a large number of fault-slip data from the mesoscale exposed faults has been recorded, in order to better understand the faulting geometry and kinematics of the region. The stress-inversion analysis of these fault-slip data in comparison with earthquake faultplane solution information permits us to define the stress regimes imposed to the region from the Late Tertiary up to the present and to correlate them with the late orogenic and post-orogenic deformation of the Hellenic orogen. In particular, five stress regimes have been defined from which the former two (D1 and D2) are related to the late collisional processes between the Apulia and Eurasia plates, the next two events (D3 and D4) are related to the present-day Hellenic subduction zone, whereas the last D5 event which is the active deformation of the region appears as an intra-continental or intra-plate deformation more related with the Adria-Eurasia ongoing convergence rather with the Hellenic subduction zone.
Λεπτομέρειες άρθρου
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Tranos, M. D., Mountrakis, D., Papazachos, C. B., Karagianni, E., & Vamvakaris, D. (2010). FAULTING DEFORMATION OF THE MESOHELLENIC TROUGH IN THE KASTORIA-NESTORION REGION (WESTERN MACEDONIA, GREECE). Δελτίο της Ελληνικής Γεωλογικής Εταιρείας, 43(1), 495–505. https://doi.org/10.12681/bgsg.11200
- Ενότητα
- Νεοτεκτονική και Γεωμορφολογία
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Λήψεις
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Αναφορές
Angelier, J., and Mechler, P. 1977. Sur une méthode graphique de recherche des contraintes principales
également utilisable en tectonique et enséismologie: la methode des diédres droits. Bull. Soc. Géol.
France, 7(19), 1309–1318.
Angelier, J., 1984. Tectonic analysis of fault slip data sets. J. Geophys. Res., 89, 5835-5848.
Brunn, J. H., 1956. Contribution á l’ étude géologique du Pinde septentrionale et d’une partie de la Macé-
doine occidentale. Annales Géologiques des Pays Helléniques, 7, 1–358.
Doutsos, T., and Kokkalas, S., 2001. Stress and deformation patterns in the Aegean region, J. Struct.
Geol., 23, 455 – 472.
Doutsos, T., G. Pe-Piper, G., Boronkay, K. and Koukouvelas, I., 1993. Kinematics of the central Hellenides.
Tectonics, 12, 936–953.
Doutsos, T., Koukouvelas, I., Zelilidis, A. and Kontopoulos, N., 1994. Intracontinental wedging and postorogenic
collapse in the Mesohellenic trough. Geol. Rundsch., 83, 257–275.
Georgiadis, G. A., Tranos, M. D. and Mountrakis, D. M., 2007. Late-and post-Alpine tectonic evolution
XLIII, No 1 – 503
of the southern part of the Athos peninsula, northern Greece. Bull. Geol. Soc. Greece, 40, 309-320.
Gephart, J. W. and Forsyth, D. W., 1984. An improved method for determining the regional stress tensor
using earthquake focal mechanism data: an application to the San Fernando earthquake sequence. J.
Geophys. Res., BS9, 9305-9320.
Le Pichon, X., and Angelier, J., 1979. The Hellenic Arc and Trench system: A key to the neotec-tonic evolution
of the eastern Mediterranean area. Tectonophysics, 69, 1 – 42.
Kahle, H. G., Straub, C., Reilinger, R., McClusky, S., King, R., Hurst, K., Veis, G. and Cross, P., 1998.
The strain rate field in the eastern Mediterranean region, estimated by repeated GPS measurements.
Tectonophysics, 294, 237 – 252.
Kilias, A. A., Tranos, M. D., Papadimitriou, E. E., and Karakostas, V. G., 2008. The recent crustal deformation
of the Hellenic orogen in Central Greece; the Kremasta and Sperchios Fault Systems and their
relationship with the adjacent large structural features. Z. dt. Ges. Ge-owiss., 159/3, 533-547. DOI:
1127/1860-1804/2008/0159-0533.
Kilias, A., Tranos, M., Mountrakis, D., Shallo, M., Marto, A. and Turku, I. 2001. Geometry and kinematics
of deformation in the Albanian orogenic belt during the Tertiary. J. Geodyn., 31, 169-187.
Kontopoulos, N., Fokianou, T., Zelilidis, A., Alexiadis, C. and Rigakis, N., 1999. Hydrocarbon potential
of the middle Eocene–middle Miocene Mesohellenic piggy-back basin (central Greece): a case study.
Mar. Petrol. Geol., 16, 811–824.
McClusky, S., et al. (28 authors) 2000. Global Positioning System constraints on plate kinematics and dynamics
in the eastern Mediterranean and Caucasus. J. Geophys. Res., 105, 5695-5719.
McKenzie, D.P. 1970. The plate tectonics of the Mediterranean region. Nature, 226, 239-243.
McKenzie, D.P. 1972. Active tectonics of the Mediterranean region. Geophys. J. R. astr. Soc., 30, 109-185.
Mercier, J. L., Simeakis, K., Sorel, D., and Vergely, P., 1989. Extensional tectonic regimes in the Aegean
basins during the Cenozoic. Basin Research, 2, 49–71.
Mountrakis, D. 1986. The 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, 335-347.
Mountrakis, D., Pavlides, S., Zouros, N., Chatzipetros, A. and Kostopoulos, D., 1996. The 13 May 1995
Western Macedonia (Greece) earthquake. Preliminary results on the seismic fault geometry and kinematics.
Proceedings of the XV Congress of the Carpatho-Balkan Geological Association, Seismicity
of the Balkan region, 112-121.
Mountrakis, D., 2006. Tertiary and Quaternary tectonics of Greece, in Dilek, Y., Pavlides, S., eds., Postcollisional
tectonics and magmatism in the Mediterranean region and Asia. Geological Society of
America, Special Paper, v. 409, p. 125-136. DOI: 10.1130/2006.2409(07).
Mountrakis, D., Tranos, M., Papazachos, C., Thomaidou, E., Karagianni, E., and Vamvakaris, D., 2006.
New neotectonic and seismological data about the main active faults and stress regime of Northern
Greece. J. Geol. Soc., London, Sp. Publ., 260, 649-670.
Papazachos, B. C., Karakostas, B. G., Kiratzi, A. A., Papadimitriou, E. E. and Papazachos, C. B., 1998a.
Basic properties of the faulting which caused the 1995 Kozani-Grevena seismic sequence. J. Geodyn.,
, 217-231.
Papazachos, B.C., Papadimitriou, E.E., Kiratzi, A.A., Papazachos, C.B. and Louvari, E.K., 1998b. Fault
plane solutions in the Aegean Sea and the surrounding area and their tectonic implications, Boll. Geof.
Teor. Appl., 39, 199-218.
Papazachos, B., Mountrakis, D., Papazachos, C., Tranos, M., Karakaisis, G. & Savvaidis, A. 2001. The
faults which have caused the known major earthquakes in Greece and surrounding region between the
th century BC and today. Proceedings of the 2nd Panhellenic Congress of Earthquake Engineering and
XLIII, No 1 – 504
Engineering Seismology, 28–30 September. Technical Chamber of Greece, Thessaloniki, 1, 17–26.
Papazachos, B., and Papazachou, C., 2003. The Earthquakes of Greece. Editions Ziti, Thessaloniki, 1-317.
Papazachos, C.B., Kiratzi, A.A. and Papazachos, B.C., 1992. Rates of active crustal deformation in the
Aegean and the surrounding area. J. Geodyn., 16, 147-179.
Papazachos, C.B. and Kiratzi, A.A., 1998. A detailed study of the active crustal deformation in the Aegean
and surrounding area. Tectonophysics, 253, 129-153.
Pavlides, S. and Mountrakis, D., 1987. Extensional tectonics of north-west Macedonia, Greece, since the
Late Miocene. J. Struct. Geol., 9, 385–392.
Reiter, F. and Acs, P., 2003. TectonicsFP software. http://www.tectonicsfp.com.
Reilinger, R. E., McClusky, S. C., Oral, M. B., King, R. W., Toksoz, M. N., Barka, A. A., Kinik, I., Lenk,
O. and Sanli, I., 1997. Global positioning system measurements of present crustal movements in the
Arabia-Africa-Eurasia plate collision zone. J. Geophys. Res., 102, 9983–9999.
Tranos, M. D., 1998. Contribution to the study of the neotectonic deformation in the region of Central
Macedonia and North Aegean. PhD. Thesis, University of Thessaloniki, (in Greek with extended
English abstract).
Tranos, M.D., 2009. Faulting of Lemnos Island; a mirror of faulting of the North Aegean Trough (Northern
Greece). Tectonophysics, 467, 72−88, DOI: 10.1016/j.tecto.2008.12.018.
Tranos, M. D., Kachev, V. N., and Mountrakis, D. M., 2008. Transtensional origin of the NE-SW Simitli
basin along the Strouma (Strymon) Lineament, SW Bulgaria. J. Geol. Soc. London, 165, 499-510, doi:
1144/0016−76492007−089
Τranos, M. D., Eleftheriadis, G. E., Kilias, A. A., 2009. Philippi granitoid as a proxy for the Oligocene
and Miocene crustal deformation in the Rhodope Massif (Eastern Macedonia, Greece). Geotectonic
Research, 96, 69-85.
Tranos, M. D. and Mountrakis, D. M., 1998. Neotectonic joints of Northern Greece: their signi-ficance
on the understanding of the active deformation. Bull. Geol. Soc. Greece, 32, 209-219.
Vamvaka, A., Kilias, A., Mountrakis, D. and Papaoikonomou, J., 2006. Geometry and structural evolution
of the Mesohellenic Trough (Greece): a new approach. J. Geol. Soc. London, Sp. Publ., 260,
-538, doi: 10.1144/GSL.SP.2006.260.01.22
Zelilidis, A., Piper, D. J. W. and Kontopoulos, N., 2002. Sedimentation and basin evolution of the
Oligocene–Miocene Mesohellenic basin, Greece. AAPG Bulletin, 86, 161–182.
