Results 11 to 20 of about 239 (95)
Cretaceous Research, 2021 Lycian Nappes (in SW Turkey) lie between the Menderes Massif and Bey Daglan carbonates and comprise thrust sheets (nappes piles) of Paleozoic-Cenozoic rocks, ophiolitic and tectonic melanges and serpentinized peridodites.
SAGULAR, Enis Kemal +5 more
core +7 more sources
Emplacement age and direction of the Lycian nappes in the Soke-Selcuk region, western Turkey
International Journal of Earth Sciences, 2001 In 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
Erdogan, B, GÜNGÖR, TALİP
core +4 more sources
Geologia Croatica, 2010 For the first time. a deep-water Lower Carbon iferous siliciclasticturbidite-olistostrome unit with many lydites (partly distally turbiditic) can be dated in the Incirbeleni Formation of the Tavas Nappe (Lycian nappes) in southwestern Turkey.
Heinz W. Kozur +2 more
doaj +2 more sources
Occurrences of Chert in Jurassic-Cretaceous Calciturbidites (SWTurkey)
Open Geosciences, 2015 The Lycian Nappes, containing ophiolite andsedimentary rocks sequences, crop out in the southwestTurkey. The Tavas Nappe is a part of the Lycian Nappes.It includes the Lower Jurassic-Upper Cretaceous calciturbidites.Chert occurrences were observed in the
Gül Murat
doaj +2 more sources
Exhumation paths of high-pressure-low-temperature metamorphic rocks from the Lycian Nappes and the Menderes massif (SW Turkey) : a multi-equilibrium approach [PDF]
Journal of Petrology, 2004 The Menderes Massif and the overlying Lycian Nappes occupy an extensive area of SW Turkey where high-pressure-low-temperature metamorphic rocks occur. Precise retrograde P-T paths reflecting the tectonic mechanisms responsible for the exhumation of these
Jolivet, L +17 more
core +5 more sources
TECTONO-SEDIMENTARY EVOLUTION OF THE EOCENE TRANSGRESSIVE DEPOSITS IN THE ACIGÖL, BURDUR AND ISPARTA AREAS (SW TURKEY) [PDF]
Acta Geographica Debrecina. Landscape & Environment Series, 2010 The Eocene transgressive deposits of the Acıgöl, Burdur and Isparta basins are the best exposed of the SW Turkey and shed light on one of the outstanding problems of the tectono-sedimentary evolution during paleotectonic and neotectonic period.
EZHER TOKER, FUZULI YAĞMURLU
doaj +2 more sources
Sedimentary Geology, 2008 Alluvial fan to shallow-marine sedimentation in the Aci{dotless}payam piggy-back basin took place in the hinterland zone of the SE-facing Lycian nappe stack and constrains the age and style of late-stage advance of these nappes.
Alçiçek, Mehmet Cihat, ten Veen, J.H.
core +6 more sources
, 2013 The idea of a continuum between the Hellenides and the Taurides is based on correlations between the platform series of the external parts of the Hellenides-Taurides system, as well as similarities between sedimentary sequences in southwestern Turkey and
Kozur, Heinz W. +6 more
core +2 more sources
, 2005 West Anatolien, welches die östliche laterale Verlängerung der ägäischen Domäne darstellt, besteht aus mehreren tektono-metamorphen Einheiten, die Hochdruck/Niedrigtemperatur (HP/LT) Gesteine aufweisen.
Rimmelé, Gaëtan
core +2 more sources
The nature and origin of magnetic anomalies over the Gölcük caldera; Isparta; South-Western Turkey
Геофизический журнал, 2018 For the first time; ground magnetic survey was performed which data were inverted by means of total horizontal derivative; horizontal gradient analytic signal; and hyperbolic tilt angle techniques to identify subsurface volcanic structures around ...
M. N. Dolmaz +4 more
doaj +1 more source