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Western Anatolia that represents the eastward lateral continuation of the Aegean domain is composed of several tectono-metamorphic units showing occurrences of high-pressure/low-temperature (HP-LT) rocks. While some of these metamorphic rocks are vestiges of the Pan-African or Cimmerian orogenies, others are the result of the more recent Alpine ...
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Mesozoic sedimentary and tectonic evolution of the Northeast Antalya Complex, Egridir, S.W. Turkey [PDF]
Waldron, John W. F.
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Focal mechanisms of small-moderate earthquakes in Denizli Graben (SW Turkey) [PDF]
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Palaeomagnetic studies of the Mesozoic-Tertiary tectonic evolution of Cyprus, Turkey and Greece [PDF]
Morris, A.
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Mesoscopic and microscopic structures along the contact between Menderes massif and Lycian nappes
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Plio-quaternary sediments and neotectonics of the Isparta angle, S.W. Turkey [PDF]
Glover, Clare Paula
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Emplacement age and direction of the Lycian nappes in the Söke-Selçuk region, western Turkey
International Journal of Earth Sciences, 2001In the Soke-Selcuk region, western Turkey, the northernmost exposures of the Lycian nappes are found as tectonic slices on the Menderes Massif. The Menderes Massif is represented by a continuous platform sequence and a blocky unit. The lower parts of the Menderes platform sequence is composed of Triassic–Jurassic marbles and an alternation of ...
GÜNGÖR, TALİP, Erdoǧan, B.
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