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Journal ArticleDOI

Late Cainozoic geodynamic evolution of Thessaly and surroundings (central-northern Greece)

TLDR
In this article, the geotectonic evolution of the Thessaly region (central-northern Greece) has been examined, using a quantitative and qualitative structural analysis; stratigraphie, sedimentological, morphotectology and seismological data.
About
This article is published in Tectonophysics.The article was published on 1993-08-15. It has received 132 citations till now. The article focuses on the topics: Basin and range topography & African Plate.

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Citations
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Journal ArticleDOI

The continuity of active fault systems in Greece

TL;DR: In this paper, the authors show that most of the active faulting in mainland Greece and the north Aegean Sea is concentrated into a small number of discrete linear zones that bound relatively rigid blocks.
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Magnitude versus faults' surface parameters: quantitative relationships from the Aegean Region

TL;DR: In this paper, a list of all earthquakes where the surface rupture length (SRL), the maximum vertical displacement (MVD) or the average displacement (AD) is available is compiled, showing good correlation coefficients equal to 0.84 and 0.82, respectively.
Journal ArticleDOI

Map view restoration of Aegean–West Anatolian accretion and extension since the Eocene

TL;DR: In this article, the authors provided the first detailed kinematic restoration of the Aegean region since 35-Ma by reconstructing up to 400 km of trench-perpendicular extension in two stages.
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Revision of the timing, magnitude and distribution of Neogene rotations in the western Aegean region

TL;DR: In this article, the authors evaluate the rotation of the clockwise rotating domain and the nature of the structures that accommodate the rotating domain in the western Aegean region, and show that the rotation covers an area including the external Albanides, western mainland Greece including Evia and probably at least partly the Peloponnesos.
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Stress and deformation patterns in the Aegean region

TL;DR: In this article, the authors present fault-slip data from about 900 faults, and summarise the structural analyses of five key structural "provinces" of the Aegean region.
References
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Journal ArticleDOI

Extensional collapse of orogens

John F. Dewey
- 01 Dec 1988 - 
TL;DR: The extensional collapse of orogens offers a partial explanation for why oceans cyclically close and reopen in roughly the same places, preservation of very high pressure metamorphic rocks, for the return of orogenic large crustal thicknesses to normal without very much erosional denudation.
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Active tectonics of the Alpine—Himalayan belt: the Aegean Sea and surrounding regions

TL;DR: In this article, the authors show that rapid extension is now taking place in the northern and eastern parts of the Aegean sea region and that the seafloor has been stretched by a factor of two since the Miocene.
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The hellenic arc and trench system: A key to the neotectonic evolution of the eastern mediterranean area

TL;DR: In this paper, the authors used the fault plane mechanisms of shallow earthquakes along the Hellenic arc and the extent of the intermediate seismic belt to make a quantitative estimate of the relative motion occurring between the Hellenians arc and adjacent sea floor.
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Aegean and surrounding regions: Complex multiplate and continuum tectonics in a convergent zone

TL;DR: The tectonics of the Aegean region involves complex slip patterns across the boundaries of several microplates that segment the end of the Anatolian plate, which is moving in a westward direction from the Bitlis zone, an intracontinental suture zone, to consume oceanic lithosphere in the eastern Mediterranean as discussed by the authors.
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Brittle microtectonics: principles and practice

TL;DR: In this paper, the authors defined the application of mesofracture analysis to the solution of tectonic problems and classified joints into fracture-system architecture and symmetry, surface morphology, dihedral angles and thin section characteristics.
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