Abstract
The Mount Athos Peninsula is situated in the south-easternmost part of the Chalkidiki Peninsula in northern Greece. It belongs to the Serbo-Macedonian Massif (SMM), a large basement massif within the Internal Hellenides. The south-eastern part of the Mount Athos peninsula is built by fine-grained banded biotite gneisses and migmatites forming a domal structure. The southern tip of the peninsula, which also comprises Mount Athos itself, is built by limestone, marble and low-grade metamorphic rocks of the Chortiatis Unit. The northern part and the majority of the western shore of the Mount Athos peninsula are composed of highly deformed rocks belonging to a tectonic mélange termed the Athos-Volvi-Suture Zone (AVZ), which separates two major basement units: the Vertiskos Terrane in the west and the Kerdillion Unit in the east. The rock-types in this mélange range from metasediments, marbles and gneisses to amphibolites, eclogites and peridotites. The gneisses are tectonic slivers of the adjacent basement complexes. The mélange zone and the gneisses were intruded by granites (Ierissos, Ouranoupolis and Gregoriou). The Ouranoupolis intrusion obscures the contact between the mélange and the gneisses. The granites are only slightly deformed and therefore postdate the accretionary event that assembled the units and created the mélange. Pb–Pb- and U–Pb-SHRIMP-dating of igneous zircons of the gneisses and granites of the eastern Athos peninsula in conjunction with geochemical and isotopic analyses are used to put Athos into the context of a regional tectonic model. The ages form three clusters: The basement age is indicated by two samples that yielded Permo-Carboniferous U–Pb-ages of 292.6 ± 2.9 Ma and 299.4 ± 3.5 Ma. The main magmatic event of the granitoids now forming the gneiss dome is dated by Pb–Pb-ages between 140.0 ± 2.6 Ma and 155.7 ± 5.1 Ma with a mean of 144.7 ± 2.4 Ma. A within-error identical age of 146.6 ± 2.3 Ma was obtained by the U–Pb-SHRIMP method. This Late Jurassic age is also known from the Kerdillion Unit and the Rhodope Terrane. The rather undeformed granites are interpreted as piercing plutons. The small granite stocks sampled have Late Cretaceous to Early Tertiary ages of 66.8 ± 0.8 Ma and 68.0 ± 1.0 Ma (U–Pb-SHRIMP)/62.8 ± 3.9 Ma (Pb–Pb). The main accretionary event was according to these data in the Late Jurassic since all younger rocks show little or no deformation. The age distribution together with the geochemical and isotopic signature and the lithology indicates that the eastern part of the Mount Athos peninsula is part of a large-scale gneiss dome also building the Kerdillion Unit of the eastern SMM and the Rhodope Massif. This finding extends the area of this dome significantly to the south and indicates that the tectonic boundary between the SMM and the Rhodope Massif lies within the AVZ.
Similar content being viewed by others
References
Anders B (2005) The Pre-Alpine evolution of the basement of the Pelagonian zone and the Vardar zone, Greece. PhD thesis, Johannes Gutenberg-Universität, Mainz, pp 1–153
Anders B, Reischmann T, Kostopoulos D (2007) Zircon geochronology of basement rocks from the Pelagonian Zone, Greece: constraints on the pre-Alpine evolution of the westernmost Internal Hellenides. Int J Earth Sci (Geol Rundsch). 96:639–661
Bébien J, Michard A, Montigny R, Feinberg H, Voidomatis P (2001) The grigoriou plutonic complex (Mt Athos, Greece): a component of the North Aegean Eocene-Oligocene Calc-Alkaline magmatism. EUG XI, Symposium LS03:314
Bonev N, Dilek Y (2009) Geochemistry and tectonic significance of proto-ophiolitic metamafic units from the Serbo-Macedonian and western Rhodope massifs (Bulgaria-Greece). Int Geol Rev. doi:10.1080/00206810902757214
Bouseley AM, Sokkary AA (1975) The relation between Rb, Ba and Sr in granitic rocks. Chem Geol 16:207–219
Brun J-P, Sokoutis D (2004) North Aegean extension: from the Rhodope core complex to Neogene basins. 5th international symposium on eastern Mediterranean geology, Thessaloniki, Greece, 14–20 April, 2004, Ref: T1–26
Brun J-P, Sokoutis D (2007) Kinematics of the southern Rhodope core complex (North Greece). Int J Earth Sci (Geologische Rundschau) 96:1079–1099
Burg J-P, Ricou L-E, Ivanov Z, Godfriaux I, Dimov D, Klain L (1993) Crustal-scale thrust complex in the Rhodope. Structure and kinematics. Bull Geol Soc Greece XXVIII/1:71–85
Burg J-P, Godfriaux I, Ricou L-E (1995) Extension of the Mesozoic Rhodope thrust units in the Vertiskos-Kerdillion Massifs (Northern Greece). C R Acad Sci Paris 320(9):889–896
Burg J-P, Ricou L-E, Ivanov Z, Godfriaux I, Dimov D, Klain L (1996) Syn-metamorphic nappe complex in the Rhodope Massif. Structure and kinematics. Terra Nova 8:6–15
Christofides G, D’Amico C, Del Moro A, Eleftheriadis G, Kyriakopoulos C (1990) Rb-Sr-geochronology and geochemical characters of the Sithonia plutonic complex (Greece). Eur J Mineral 2:79–87
Christofides G, Perugini D, Koroneos A, Soldatos T, Poli G, Eleftheriadis G, Del Moro A, Neiva AM (2007) Interplay between geochemistry and magma dynamics during magma interaction: an example from the Sithonia Plutonic Complex (NE Greece). Lithos 95:243–266. doi:10.1016/j.lithos.2006.07015
Compston W, Williams IS, Meyer C (1984) U-Pb geochronology of zircons from lunar breccia 73217 using a sensitive high mass-resolution ion microprobe. J Geophys Res 89(supplement):B525–B534
De La Roche H, Leterrier J, Grandeclaude P, Marchal M (1980) A classification of volcanic and plutonic rocks using R1–R1 diagrams and major and trace element analysis—its relationship to modern nomenclature. Chem Geology 29:183–210
De Wet AP (1989) Geology of a part of the Chalkidiki peninsula, Northern Greece. PhD thesis, Cambridge University, pp 1–177
De Wet AP, Miller JA, Bickle MJ, Chapman HJ (1989) Geology and geochronology of the Arnea, Sithonia and Ouranoupolis intrusions, Chalkidiki peninsula, Northern Greece. Tectonophysics 161:65–79
Dimitriadis S, Godelitsas A (1991) Evidence for high pressure metamorphism in the Vertiskos group of the Serbomacedonian Massif: the eclogite of Nea Roda, Chalkidiki. Bulletin of the Geological Society of Greece XXV/2:67–80
Dimitrijevic, MD (1997) Geology of Yugoslavia. Special publication—Geological Institute GEMINI, Belgrade, 187 pp
Dinter DA, Royden L (1993) Late Cenozoic extension in northeastern Greece; Strymon Valley detachment system and Rhodope metamorphic core complex. Geology 21(1):45–48
Dinter DA, Macfarlane A, Hames W, Isachsen C, Bowring S, Royden L (1995) U-Pb and 40Ar/39Ar geochronology of the symvolon granodiorite: implications for the thermal and structural evolution of the Rhodope metamorphic core complex, northeastern Greece. Tectonics 14(4):886–908
Dixon JE, Dimitriadis S (1984) Metamorphosed ophiolitic rocks from the Serbo-Macedonian Massif, near lake Volvi, North-east Greece. In: Dixon JE, Robertson AHF (eds) The geological evolution of the eastern Mediterranean. Geol Soc London Special Publ 17:603–618
Frei R (1996) The extend of inner mineral isotope equilibrium: a systematic bulk U-Pb and Pb step leaching (PbSL) isotope study of individual minerals from a Tertiary granite of lerissos (northern Greece). Eur J Miner 8:1175–1189
Georgiadis GA, Tranos MD, Mountrakis DM (2007) Late- and post-alpine tectonic evolution of the southern part of the Athos peninsula, northern Greece. Bull Geol Soc Greece XXXX:309–321
Gumann S, Lahaye Y, Brey G (2003) Iridium strip–Rhyolithe enthüllen ihre details. Ber Eur Jb Min 15:72
Himmerkus F, Reischmann T, Kostopoulos DK (2003) The Serbo-Macedonian Massif, the oldest crustal segment of the internal Hellenides, identified by zircon ages. Geophys Res Abstr 5:05671
Himmerkus F, Zachariadis P, Reischmann T, Kostopoulos DK (2005) The mafic complexes of the Athos-Volvi-Zone—a suture zone between the Serbo-Macedonian Massif and the Rhodope Massif? Geophys Res Abstr 7:10240
Himmerkus F, Anders B, Reischmann T, Kostopoulos DK (2007) Gondwana-derived terranes in the northern Hellenides. In: Hatcher RD Jr, Carlson MP, McBride JH, Martínez-Catalán JR (eds), 4-D Framework of Continental Crust. Geol Soc Am Memoir 200(19):379–390. doi:10.1130/2007.1200
Himmerkus F, Reischmann T, Kostopoulos DK (2009a) Serbo-Macedonian revisited: a Silurian basement terrane from northern Gondwana in the internal Hellenides, Greece. Tectonophysics. doi:10.1016/j.tecto.2008.10.016
Himmerkus F, Reischmann T, Kostopoulos DK (2009b) Triassic rift-related meta-granites in the Internal Hellenides, Greece. Geol Mag 146(2):252–265. doi:10.1017/S001675680800592X
Kober B (1986) Whole grain evaporation for 207Pb/206Pb-age investigations on single zircons using a double filament thermal ion source. Contrib Miner Petrol 93:482–490
Kober B (1987) Single zircon evaporation combined with Pb+emitter-bedding for 207Pb/206Pb-age investigations using thermal ion mass spectrometry, and implications to zirconology. Contrib Miner Petrol 96:63–71
Kockel F, Mollat H, Walther HW (1977) Erläuterungen zur geologischen Karte der Chalkidiki und angrenzender Gebiete 1:100000 (Nord-Griechenland). Bundesanstalt für Geowissenschaften und Rohstoffe, Hannover, pp 1–119
Kockel F, Walther HW (1965) Die Strimonlinie als Grenze zwischen Serbo-Mazedonischen und Rila-Rhodope-Massif in Ost-Mazedonien. Geol Jb 83:575–602
Kockel F, Mollat H, Walther HW (1971) Geologie des Serbo-Mazedonischen Massivs und seines mesozoischen Rahmens (Nordgriechenland). Geol Jb 89:529–551
Le Maitre RW (1989) A classification of igneous rocks and glossary of terms. Blackwell Sci Publ, Oxford, pp 1–193
Liati A, Fanning MC (2005) Eclogites and country rock orthogneisses representing upper Permian Gabbros in Hercynian Granitoids, Rhodope, Greece: geochronological constraints. Mitteilungen der Österreichischen Mineralogischen Gesellschaft 150:88
Lips ALW, White SH, Wijbrans JR (2000) Middle-late Alpine thermostatic evolution of the southern Rhodope Massif, Greece. Geodin Acta 13:281–292
Meinhold G, Kostopoulos D, Reischmann T, Frei D, BouDagher-Fadel MK (2009a) 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
Meinhold G, Kostopoulos DK. Frei, D Himmerkus F, Reischmann T (2009b) U–Pb LA-SF-ICP-MS zircon geochronology of the Serbo-Macedonian Massif, Greece: palaeotectonic constraints for Gondwana-derived terranes in the Eastern Mediterranean. Int J Earth Sci (Geol Rundsch). doi:10.1007/s00531-009-0425-5
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 Geology 94:335–347
Papanikolaou D (1997) The tectonostratigraphic terranes of the Hellenides. Ann Géol Pays Hellén 37:495–514
Papanikolaou D (2009) Timing of tectonic emplacement of the ophiolites and terrane paleogeography in the Hellenides. Lithos 108:262–280. doi:10.1016/j.lithos.2008.08.003
Papanikolaou D, Panagopoulos A (1981) On the structural style of Southern Rhodope. Geol Balc 11(3):13–22
Pearce JA, Harris NBW, Tindle AG (1984) Trace element discrimination diagrams for the tectonic interpretation of granitic rocks. J Petrology 25:956–983
Peytcheva I, von Quadt A (1995) U–Pb Zircon dating of metagranites from Byala Reka region in the east Rhodopes, Bulgaria. Geol Soc Greece Sp Publ 4:637–642
Ricou L-E, Burg J-P, Godfriaux I, Ivanov Z (1998) Rhodope and Vardar: the metamorphic and the olistostromic paired belts related to the Cretaceous subduction under Europe. Geodin Acta 11:285–309
Sokoutis D, Brun JP, Van den Driessche J, Pavlides S (1993) A major Oligo-Miocene detachment in southern Rhodope controlling north Aegean extension. J Geol Soc Lond 150:243–246
Spiess R, Cesare B, Mazzoli C, Sassi R, Sassi FP (2010) The crystalline basement of the Adria microplate in the eastern Alps: a review of the palaeostructural evolution from the Neoproterozoic to the Cenozoic. Rend Fis Acc Lincei 21(Suppl 1):S31–S50. doi:10.1007/s12210-010-0100-6
Stacey JS, Kramers J (1975) Approximation of terrestrial lead isotope evolution by a two stage model. Earth Planet Sci Lett 26:207–221
Stampfli GM, Borel GD (2002) A plate tectonic model for the Paleozoic and Mesozoic constrained by dynamic plate boundaries and restored synthetic oceanic isochrones. Earth Planet Sci Lett 196:17–33
Turpaud P (2006) Characterization of igneous terranes by zircon dating: implications fort he UHP relicts occurrences and suture identification in the central Rhodope, Northern Greece. PhD thesis, Johannes Gutenberg-Universität Mainz, pp 1–107
Turpaud P, Reischmann T (2003) Zircon ages of granitic gneisses from the Rhodope (N. Greece), determination of basement age and evidences for a Cretaceous intrusive event. Geophys Res Abstr 5:04435
Turpaud P, Reischmann T (2009) Characterisation of igneous terranes by zircon dating: implications for UHP occurrences and suture identification in the Central Rhodope, northern Greece. Int J Earth Sci (Geol Rundsch). doi:10.1007/s00531-008-0409-x
von Raumer JF, Stampfli GM (2008) The birth of the Rheic Ocean—Early Palaeozoic subsidence patterns and subsequent tectonic plate scenarios. Tectonophysics 461:9–20
von Raumer JF, Stampfli GM, Bussy F (2003) Gondwana-derived microcontinents–the constituents of the Variscan and Alpine collisional orogens. Tectonophysics 365:7–22
White WM, Patchett J (1984) Hf-Nd-Sr isotopes and incompatible element abundances in island arcs: implications for magma origins and crust-mantle evolution. Earth Planet Sci Lett 67:167–185
Williams IS (1992) Some observations on the use of zircon U-Pb geochronology in the study of granitic rocks. Trans R Soc Edinb Earth Sci 83:447–458
Acknowledgments
This work would have been impossible without the written consent of the Holy Supervision Committee of the State of Athos. F. Himmerkus and P. Zachariadis would like to thank the Deutsche Forschungsgemeinschaft and the county of Rheinland Pfalz for funding of the project of the Graduiertenkolleg “Stoffbestand und Entwicklung von Kruste und Mantel”. Also thanks to P. Turpaud and G. Meinhold for useful discussions. We greatly appreciate the technical assistance provided by N. Goschopf and B. Schulz-Dorbrick (XRF), J. Huth (CL-Pictures) and W. Todt, U. Poller and I. Raczek (laboratory and TIMS). We would like to thank the organisation committee of “Ophiolites 2008” for the great job they did. Sarantis Dimitriadis and John Dixon strongly improved the manuscript with their comments and suggestions.
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
About this article
Cite this article
Himmerkus, F., Zachariadis, P., Reischmann, T. et al. The basement of the Mount Athos peninsula, northern Greece: insights from geochemistry and zircon ages. Int J Earth Sci (Geol Rundsch) 101, 1467–1485 (2012). https://doi.org/10.1007/s00531-011-0644-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s00531-011-0644-4