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Die mesozoisch-tertiaren Serien der Argolis-Halbinsel sind In der externen Adhami-Basalsequenz wird die Radiolarit in ein mehrphasiges Deckengebaude einbezogen, in dem sich Formation von Ophiolith fUhrenden lithischen Kalkareni zwei tertiar-tektonische {laquo}Composite Units{raquo} und die Akros ten und schliesslich von groben, mehrere 100 m machtigen Decke unterscheiden lassen. Beide {laquo}Composite Units{raquo} set Hornstein-Kalk-Breccien iiberlagert (Kandhia Breccia). Die zen sich aus einer Basalsequenz und im Spat jura darauf Komponenten stammen hauptsachlich aus der tektonisch iiberschobenen Deckeneinheiten zusammen. Die Adhami auflagernden Asklipion-Decke. Die Kandhia-Breccie er {laquo}Composite Unit{raquo} als externe und die Dhidhimi-Trapezona brachte Radiolarienfaunen des Tithonian. {laquo}Composite Unit{raquo} als interne Einheit unterscheiden sich Die Asklipion-Decke umfasst eine Tiefwasserserie, begin durch eine zeitlich und faziell verschiedene oberjurassische nend mit untertriadischen sauren Vulkaniten, gefolgt von klastische Faziesentwicklung in der Basalsequenz wie auch bis zu 1000 m machtigen Hornstein-Plattenkalken, die sich durch einen verschiedenen Gesteinsinhalt der iiberlagernden bis in den Lias fortsetzen. Diese Serie wird ebenfalls von, spat jurassischen Decken. Die Entwicklung von Plattform hier mitteI- bis oberjurassischen Radiolariten (Koliaki zu peJagischer Sedimentation erfolgte in beiden Basal Chert) und einer Ophiolith-Klasten fUhrenden, zunehmend sequenzen zunachst auf ahnliche Weise: Obertriadische bis grobkornigeren klastischen Serie iiberlagert. Die mittel-/ mittelliasische Flachwasserkalke (Pantokrator-Kalk) wer obertriadischen Asklipion-Kalke treten als verkehrt liegende den im ganzen Gebiet von pelagischen Kalken iiberlagert.
The Mediterranean region represents a complex mosaic of continental, microcontinental and ophiolitic terranes, whose overall evolution has been controlled by relative movements between the African and Eurasian plates. Palaeomagnetic studies have played an important part in deciphering the sequence of tectonic events in this region. The 33 papers presented here span the full width of the Mediterranean basin and present results from Permian to Quaternary rocks.
A hill dominating the Nemea Valley, Tsoungiza is located only 10 kilometers northwest of the citadel of Mycenae. Excavations there have uncovered the remains of a Late Helladic settlement that stood at its southern end. This volume presents the results of these investigations with an unprecedented study of a small settlement's economy and society in the Mycenaean period. Through an interdisciplinary approach that incorporates a wide variety of general and specialist studies, the authors demonstrate how agricultural production, craft activities, and ceremonial practices integrated the inhabitants of Tsoungiza into a regional exchange system within the Bronze Age world. The volume includes contributions by P. Acheson, S. E. Allen, K. M. Forste, P. Halstead, S. M. A. Hoffmann, A. Karabatsoli, K. Kaza-Papageorgiou, B. Lis, R. Mersereau, H. Mommsen, J. B. Rutter, T. Theodoropoulou, and J. E. Tomlinson.
The Eastern Mediterranean region is a classic area for the study of tectonic processes and settings related to the development of the Tethyan orogenic belt. The present set of research and synthesis papers by earth scientists from countries in this region and others provides an up-to-date, interdisciplinary overview of the tectonic development of the Eastern Mediterranean region from Precambrian to Recent. Key topics include continental rifting, ophiolite genesis and emplacement, continental collision, extensional tectonics, crustal exhumation and intra-plate deformation (e.g. active faulting). Alternative tectonic reconstructions of the Tethyan orogen are presented and discussed, with important implications for other regions of the world. The book will be an essential source of information and interpretation for academic researchers (geologists and geophysicists), advanced undergraduates and also for industry professionals, including those concerned with hydrocarbons, minerals and geological hazards (e.g. earthquakes).
This 2-volume set provides a state-of-the-art study of the fossil record and taxonomy of the main vertebrate groups from Greece. Greece stands between 3 continents and its vertebrate fossil record is of great importance for paleontological and evolutionary studies in Europe, Asia and Africa. Fossils from classic, world-famous localities (e.g., Pikermi, Samos) form an essential part of the collections of the most important museums in the world and have been studied by numerous scientists. Recent paleontological research led to the discovery and study of numerous new sites. The volumes contain a taxonomic review of all named and identified taxa, their taxonomic history and current status, as well as historical, phylogenetic and biogeographic information. Volume 1 contains a synopsis of the fossil record and taxonomy of important groups of vertebrates represented in the fossil record of Greece. The volume deals with some of the early splitting clades, including the basal and enigmatic conodonts and basal tetrapods like fishes, amphibians, and reptiles like lizards, snakes, crocodiles, turtles and tortoises. The second part of the volume deals with basal mammalian clades, some of which are quite characteristic for the fossil record of the country: aardwarks, hyraxes, proboscideans, elephants and mammoths, sea cows, rodents, and lagomorphs. The volume ends with special chapters on the primate fossil record of the country, including some of our most recent and distant relatives.