Results 41 to 50 of about 1,426 (164)
Clay mineralogy, chemistry, and diagenesis of late devonian K-bentonite occurrences in northwestern Turkey [PDF]
, 2015 Thin beds of tephra (K-bentonites) formed by the diagenesis of volcanic ash are exposed within the limestone-dolomitic limestone successions of the Yilanli formation at Zonguldak and Bartin in northwestern Turkey.
Bozkaya, Ömer +5 more
core +1 more source
Was the Formation of the North Anatolian Fault Influenced by the Aegean Extension?
Terra Nova, Volume 37, Issue 5, Page 342-352, October 2025.ABSTRACT The North Anatolian Fault (NAF), one of the most prominent plate boundary continental fault systems on Earth, facilitates the westward movement of the Anatolian microplate into the Aegean region. The temporal and spatial evolution of the NAF is important for understanding the mechanism of escape tectonics during plate interaction in active ...
I. Tonguç Uysal +9 more
wiley +1 more source
Pre‐Rift Orogenic Erosion Facilitates the Exhumation of Lower Crust at Rifted Margins
Geophysical Research Letters, Volume 52, Issue 14, 28 July 2025.Abstract During the late‐stage of continental rifting, lower crustal rocks can be exhumed to the Earth's surface. Such exposure has been identified especially in rifts that developed within former orogens. These rifts exploited zones of lithospheric weakness created during previous mountain‐building events.
Kai Li +6 more
wiley +1 more source
The interaction between Aegean back-arc extension and Anatolia escape since Middle Miocene [PDF]
, 2014 International audienceThe Aegean domain is a key area for understanding the processes of back-arc extension. Observed deformation pattern and present day kinematics result from the interaction between the southward retreat of the Hellenic trench and the ...
Brun, Jean-Pierre +3 more
core +2 more sources
International Journal of Climatology, Volume 45, Issue 9, July 2025.We have compiled research published since 1980 on annual precipitation trends in the Mediterranean basin. A total of 337 papers were analysed, with the aim of providing a comprehensive overview of the available research, rather than evaluating the quality of the data, methods, or interpretations.
José Carlos González‐Hidalgo +1 more
wiley +1 more source
Lithospheric Unzipping Explaining Hot Orogenesis During Continental Subduction
Tectonics, Volume 44, Issue 7, July 2025.Abstract Phanerozoic accretionary orogens typically contain upper crustal nappes derived from subducted lithosphere—oceanic or continental—that display (ultra‐)high‐pressure, low‐temperature ((U)HP‐LT) metamorphism. Surprisingly, such orogens often also contain coeval continent‐derived nappes that underwent “Barrovian” (MP‐HT) syn‐burial metamorphism ...
Douwe J. J. van Hinsbergen +2 more
wiley +1 more source
Syn-tectonic sedimentary evolution of the Miocene Çatallar Basin, southwestern Turkey [PDF]
, 2009 International audienceThe Çatallar Basin is one of the Miocene basins located in the southern part of the Bey Dağları Massif (SW Turkey). This basin has been reinvestigated and new stratigraphic and sedimentological data are now presented.
Ciner, A. +4 more
core +3 more sources
Geophysical Prospecting, Volume 73, Issue 4, Page 1243-1254, May 2025.Abstract This study introduces the application of the 2D weighted compact gravity inversion technique to model crustal thickness and intracrustal discontinuities in the Aegean region, encompassing both marine and terrestrial areas over a significant area of 430 km × 333 km.
M. B. Doğan
wiley +1 more source
Stratigraphic Revision of the Selendi, Güre, and Uşak Neogene Basins, Western Anatolia
Acta Geologica Sinica - English Edition, Volume 99, Issue 2, Page 332-351, April 2025.Abstract In a re‐examination of the Neogene stratigraphy of the Uşak, Güre, and Selendi basins of western Anatolia, western Turkey, the stratigraphic position of the previously defined İnay Group is revised, which was previously considered to be of the Middle Miocene age.
Fikret GÖKTAŞ +2 more
wiley +1 more source
Etude du Kemalpaşa Dağı (Province d'İzmir, Turquie)
Bulletin of the Mineral Research and Exploration, 1963 Le Kemalpaşa Dağı est un massif calcaire de 20 km de diametre s'elevant jusqu'a 1500 m entre İzmir et les contreforts du massif cristallin de Menderes. La structure est compliquee; une orientation SW-NE predomine cependant. Des failles WE le tronquent au
Joel VERDIER
doaj