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The sedimentary expression of regional tectonic events during the Miocene-Pliocene transition in the southern Cyprus basins

Published online by Cambridge University Press:  01 May 2009

F. Orszag-Sperber
Affiliation:
Laboratoire de Pétrologie Sédimentaire et Paléontologie, Université Paris-Sud (Orsay), UA 723, 91405-Orsay Cedex, France
J. M. Rouchy
Affiliation:
Laboratoire de Géologie, Muséum National d'histoire Naturelle, UA 1209, 43 Rue Buffon, 75005 Paris, France
P. Elion
Affiliation:
Petrole Ingeneering S.A., 21 Avenue Victor Hugo, Paris, France

Abstract

A well-known tectonic event affecting the East Mediterranean region, generally referred to as ‘the’ Miocene–Pliocene phase, occurs at, or near the Miocene–Pliocene boundary. Recent sedimentological studies in Cyprus indicate that this ‘event’, in fact, is complex. The Tortonian–Lower Pliocene period is marked by a stress involving an N20 extension in the Polemi and Pissouri basins and by an N100 extension in the Psematismenos basin. Sedimentological studies have demonstrated three tectonic pulsations during Messinian time, prior to the Pliocene transgression. These are expressed by two episodes of seismic brecciation, and a palaeo-emersion is indicated by palaeosols and detrital discharges. These phenomena suggest brief tectonic instability during Messinian time. Microtectonic studies in the South Troodos basins of Cyprus reveal that the main change in tectonic stress does not coincide with the Miocene–Pliocene contact but occurs at the end of Lower Pliocene time. The authors conclude that the so-called Miocene–Pliocene ‘event’, in reality, is a series of subtle tectonic pulsations recorded clearly by sedimentary parameters.

Type
Articles
Copyright
Copyright © Cambridge University Press 1989

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References

Angelier, J. 1979. Néotectonique de l'are égéen. Société Géologique du Nord no. 3, 405 pp.Google Scholar
Baroz, F., Bizon, G., Heiman, K. O., Mallet, J. P., Muller, C., Orszag–Sperber, F., Rouchy, J. M. & Weisgerber, F. 1977. Le Miocène terminal et le Pliocène dans la région de Polémi (Chypre ouest). Milieux de dépôts. Comptes-Rendus de l'académie des Sciences de Paris 286D, 1771–4.Google Scholar
Biju-Duval, B., Courrier, P. & Letouzey, J. 1974. Interprétation de la structure des Monts de Misis Turquie (chevauchement Pliocène et masses allochtones mises en place au Miocène) et son extension en Méditerranée orientale. 2ème Réunion des Sciences de la Terre, Nancy.Google Scholar
Biju-Duval, B. & Dercourt, J. 1980. Les bassins de la Méditerranée orientale présentent-ils les restes d'un domaine océanique, la Mésogée, ouvert au Mésozoïque et distinct de la Téthys? Bulletin de la Société Géologique de France (7e sér.) 22 (1), 4360.Google Scholar
Bizon, G. & Bizon, J. J. 1976. Modalités du passage Miocène–Pliocène en Méditerranée; Réflexions sur le Messinien. Palaeogeography, Palaeoclimatology, Palaeoecology 20, 43–6.CrossRefGoogle Scholar
Garrison, R. E., Schreiber, B. C., Bernouilli, D., Fabricius, F. H., Kidd, R. B. & Melières, F. 1978. Sedimentary petrology and structures of Messinian evaporitic sediments in the Mediterranean sea, Leg 42A, DSDP. In Initial Reports of the Deep Sea Drilling Project, 42 (ed. Hsu, K.& Montadert, L. et al. ), pp. 571611. Washington: U.S. Government Printing Office.Google Scholar
Gass, F. 1960. The geology and mineral resources of Dhali area. Cyprus Geological Survey Department, Memoir no. 4, 116 pp., Nicosia.Google Scholar
Hsu, K. I., Montadert, L., Bernouilli, D., Cita, M. B., Erikson, A., Garrison, R. G., Kidd, R. B., Mélières, F., Muller, C. & Wright, R. 1978. History of the Mediterranean salinity crisis. Initial Reports of the Deep Sea Drilling Project 42 (1), Washington: U.S. Government Printing Office.Google Scholar
Lapierre, H. 1975. Les formations sédimentaires et éruptives des nappes de Mamonia et leurs relations avec le massif du Troodos (Chypre). Mémoires de la Société Géologique de France, n.s. 54, 1123.Google Scholar
Letouzey, J. & Trémolières, J. 1980. Paleostress fields around the Mediterranean since the Mesozoic derived from microtectonic: comparison with plate tectonic data. Mémoires du Bureau de Recherches Géologiques et Minières, 115, 261–73.Google Scholar
McCallum, J. & Robertson, A. H. F. 1987. Pulsed uplift of the Troodos massif. Abstract, in Troodos 87: Ophiolites and Oceanic Lithosphere, Symposium, Nicosia, p. 24.Google Scholar
McKenzie, J. A., Jenkyns, H. C. & Bennett, G. G. 1979–80. Stable isotope study of the cyclic diatomiteclaystones from the Tripoli formation, Sicily: a prelude to the Messinian salinity crisis. Palaeogeography, Palaeoclimatology, Palaeoecology 29, 125–41.Google Scholar
Mercier, J. L., Delibassis, N., Gauthier, A., Jarrige, J. J., Lemeille, F., Philippe, H., Sebrier, M. & Sorel, D. 1979. La tectonique de I'arc Égéen. Revue de Géologie Dynamique et Géographic Physique 21 (1).Google Scholar
Orszag-Sperber, F. 1982. Le passage Miocène-Pliocène: une succession d'évènements géodynamiques. Abstracts, Société Géologique de France, 5ème Réunion Annuelle des Sciences de la Terre, Paris.Google Scholar
Orszag-Sperber, F. & Rouchy, J. M. (eds) 1980. Aspects géodynamiques du passage Miocène–Pliocène en Méditerranée. Géologie Méditerranéenne 7 (1), 1154.Google Scholar
Orszag-Sperber, F. & Rouchy, J. M. 1983. Un jalon dans la connaissance de l'évolution paléo-climatique à la limite Miocène–Pliocène en Méditerranée orientale: l'exemple du bassin de Pissouri (Chypre). Paléobiologie continentale (Montpellier) 14 (2), 377–83.Google Scholar
Orszag-Sperber, F., Rouchy, J. M., Bizon, G., Cravatte, J. & Muller, C. 1980. La sédimentation messinienne dans le bassin de Polemi (Chypre). Géologie Méditerranéenne, 7 (1), 91101.Google Scholar
Pantazis, T. M. 1969. Landslides in Cyprus. Geological Survey Department, Bulletin no. 4, Nicosia, 98 pp.Google Scholar
Pantazis, T. M. 1978. Cyprus evaporites, In Initial Reports of the Deep Sea Drilling Project 42 (2) (ed. Ross, D. A., Neprochnov, Y. P. et al. ), pp. 1185–94. Washington: U.S. Government Printing Office.Google Scholar
Robertson, A. H. F. 1977. Tertiary uplift history of the Troodos massif (Cyprus). Geological Society of America Bulletin 88, 1763–72.Google Scholar
Robertson, A. H. F. & Hudson, J. D. 1974. Pelagic sediments in the Cretaceous and Tertiary history of Cyprus. In Pelagic Sediments on Land and Under the Sea (ed. Hsü, K., Jenkins, H.), pp. 403–36. International Association of Sedimentologists, Special Publication no. 1.Google Scholar
Robertson, A. H. F. & Woodcock, N. H. 1980. Tectonic setting of the Troodos massif in the East Mediterranean. In Ophiolites (ed. Panayiotou, A.), pp. 3649. Symposium, Nicosia.Google Scholar
Rouchy, J. M. 1982. La genèse des évaporites messiniennes de Méditerranée. Mémoires du Muséum National d'histoire Naturelle, 50, Sér. C, 267 pp.Google Scholar
Rouchy, J. M., Orszag-Sperber, F., Bizon, G. & Bizon, J. J. 1980. Mise en évidence d'une phase d'émersion fini-messinienne dans le bassin de Pissouri (Chypre). Une modalité de passage Miocène-Pliocène en Méditerranée orientale. Comptes-Rendus de l'académie des Sciences de Paris 291, 729–32.Google Scholar
Swarbrick, R. E. & Naylor, M. A. 1980. The Kathikas mélange, SW Cyprus: late Cretaceous submarine debris flows, Sedimentology 27, 6378.CrossRefGoogle Scholar
Vaumas, E. de. 1961. Further contributions to the geomorphology of Cyprus. Cyprus Geological Survey Department, Annual Report, Nicosia.Google Scholar
Ward, L. C. 1988. The Polis basin, N.W. Cyprus. A neotectonic extensional graben of Miocene to Recent age. In The Structural and Sedimentary Evolution of the Neotectonic Aegean Basins. BSGR/TSG meeting of the Geological Society of London. Abstracts.Google Scholar
Ward, L. C. & Robertson, A. H. F. 1987. Structural and sedimentological development of the Miocene–Recent Polis extensional graben, N.W. Cyprus. Abstract in Troodos 87: Ophiolites and Oceanic Lithosphere, Symposium, Nicosia, p. 45.Google Scholar