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Relevant bibliographies by topics / Alaşehir (Turkey)

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Academic literature on the topic 'Alaşehir (Turkey)'

Author: Grafiati

Published: 1 March 2023

Last updated: 30 July 2024

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Journal articles on the topic "Alaşehir (Turkey)"

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SEYİTOĞLU, GÜROL. "Late Cenozoic tectono-sedimentary development of the Selendi and Uşak-Güre basins: a contribution to the discussion on the development of east–west and north trending basins in western Turkey." Geological Magazine 134, no. 2 (1997): 163–75. http://dx.doi.org/10.1017/s0016756897006705.

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This paper expands the K–Ar dating and palynologically controlled stratigraphical data base reported in earlier papers to the north trending Selendi and Uşak-Güre basins located to the north of east–west trending Alaşehir graben in western Turkey. These north trending basins began to form during Early Miocene times and most of their basin fills accumulated before 14 Ma, except for the youngest Asartepe formation. Recent studies of both east–west grabens and north trending basins show that they started to develop simultaneously during Early Miocene times under the north–south extensional regime, and the classification of the structures as ‘replacement’ and ‘revolutionary’ has no meaning for the Alaşehir graben and the basins located to its north.

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SEYITOĞLU, GÜROL, İBRAHIM ÇEMEN, and OKAN TEKELI. "Extensional folding in the Alaşehir (Gediz) graben, western Turkey." Journal of the Geological Society 157, no. 6 (2000): 1097–100. http://dx.doi.org/10.1144/jgs.157.6.1097.

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Seyitoğlu, Gürol, and Barry C. Scott. "Age of the Alaşehir graben (West Turkey) and its tectonic implications." Geological Journal 31, no. 1 (1996): 1–11. http://dx.doi.org/10.1002/(sici)1099-1034(199603)31:1<1::aid-gj688>3.0.co;2-s.

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Seyítoğlu, Gürol, and Barry C. Scott. "Late Cenozoic basin development in west Turkey: Gördes basin tectonics and sedimentation." Geological Magazine 131, no. 5 (1994): 631–37. http://dx.doi.org/10.1017/s0016756800012425.

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AbstractThe early Miocene sedimentary succession in the northeast-southwest trending Gördes basin is 1000 m thick and divided into the Daĝdere, Tepeköy and Kuşlukköy formations. The age of this fill can be constrained as between 24.2 Ma and 16.3 Ma, at its widest interval. Paleocurrent directions from south to north demonstrate that the basin had a north dipping basin floor. These observations are inconsistent with a previous model of the Gordes basin as a cross graben with a south dipping basin floor, towards the Alaşehir graben, and an anomalously thick (up to 3000 m) basin filling.

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Yilmaz, M., and K. Gelisli. "Stratigraphic–structural interpretation and hydrocarbon potential of the Alaşehir Graben, western Turkey." Petroleum Geoscience 9, no. 3 (2003): 277–82. http://dx.doi.org/10.1144/1354-079302-539.

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SEYİTOĞLU, GÜROL, OKAN TEKELİ, İBRAHİM ÇEMEN, ŞEVKET ŞEN, and VEYSEL IŞIK. "The role of the flexural rotation/rolling hinge model in the tectonic evolution of the Alaşehir graben, western Turkey." Geological Magazine 139, no. 1 (2002): 15–26. http://dx.doi.org/10.1017/s0016756801005969.

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The Alaşehir graben is a well-defined prominent extensional structure in western Turkey, generally trending E–W and containing four sedimentary units. At the beginning of graben formation during Early–Middle Miocene times, the first fault system was active and responsible for the accumulation of the first and second sedimentary units. In Pliocene times, a second fault system developed in the hanging wall of the first system and a third sedimentary unit was deposited. The recently active third fault system separates older graben fill and a fourth sedimentary unit. Activity on each fault system caused the rotation and uplift of previous systems, similar to the ‘flexural rotation/rolling hinge’ model, but our field observations indicate that the rotated first fault system is also active, allowing exhumation of larger amounts of rock units. This paper documents that graben formation in western Turkey is a sequential process. Its different periods are represented by three fault systems and associated sedimentation. Consequently, recent claims using age data from only the second and/or third sedimentary units to determine the timing of graben formation are misleading.

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GLODNY, JOHANNES, and RALF HETZEL. "Precise U–Pb ages of syn-extensional Miocene intrusions in the central Menderes Massif, western Turkey." Geological Magazine 144, no. 2 (2006): 235–46. http://dx.doi.org/10.1017/s0016756806003025.

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Western Turkey is an area which has experienced large-scale extension of continental crust. Here we report precise crystallization ages of two intrusions in the central Menderes Massif, the Turgutlu and Salihli granodiorites, using U–Pb dating. Both intrusions occur in the southern footwall of the seismically active Alaşehir graben and were emplaced syntectonically in an extensional top-to-the-NNE shear zone which was active at retrograde greenschist-facies conditions. The U–Pb ages of 16.1 ± 0.2 Ma (monazite, Turgutlu granodiorite) and 15.0 ± 0.3 Ma (allanite, Salihli granodiorite) document that tectonic exhumation of middle-crustal rocks in the central Menderes Massif was already underway at the Early to Middle Miocene transition. Combined with published geochronological, structural and sedimentological data, the new U–Pb ages point to a continued extension since at least 16 Ma. There is no convincing evidence for a late Miocene/Pliocene phase of tectonic shortening.

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8

Kent, E., S. J. Boulton, I. S. Stewart, A. C. Whittaker, and M. C. Alçiçek. "Geomorphic and geological constraints on the active normal faulting of the Gediz (Alaşehir) Graben, Western Turkey." Journal of the Geological Society 173, no. 4 (2016): 666–78. http://dx.doi.org/10.1144/jgs2015-121.

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Sargın, Seyid Ahmet, Ekrem Akçicek, and Selami Selvi. "An ethnobotanical study of medicinal plants used by the local people of Alaşehir (Manisa) in Turkey." Journal of Ethnopharmacology 150, no. 3 (2013): 860–74. http://dx.doi.org/10.1016/j.jep.2013.09.040.

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Gemici, Ünsal. "Evaluation of the water quality related to the acid mine drainage of an abandoned mercury mine (Alaşehir, Turkey)." Environmental Monitoring and Assessment 147, no. 1-3 (2007): 93–106. http://dx.doi.org/10.1007/s10661-007-0101-9.

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Books on the topic "Alaşehir (Turkey)"

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Taunay, Taunay Alfredo d'Escragnolle. Goyaz. Instituto Centro-Brasileiro de Cultura, 2004.

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Book chapters on the topic "Alaşehir (Turkey)"

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Bülbül, Ali, Tuğbanur Özen Balaban, and Gültekin Tarcan. "Evaluation of the Contamination from Geothermal Fluids upon Waters and Soils in Alaşehir Environs, Turkey." In Advances in Sustainable and Environmental Hydrology, Hydrogeology, Hydrochemistry and Water Resources. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-01572-5_39.

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Seyitoğlu, Gürol, Nicholas D. Cahill, Veysel Işık, and Korhan Esat. "Morphotectonics of the Alaşehir Graben with a Special Emphasis on the Landscape of the Ancient City of Sardis, Western Turkey." In World Geomorphological Landscapes. Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-030-03515-0_28.

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Fant, Clyde E., and Mitchell G. Reddish. "Philadelphia." In A Guide to Biblical Sites in Greece and Turkey. Oxford University Press, 2003. http://dx.doi.org/10.1093/oso/9780195139174.003.0043.

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The ancient city of Philadelphia is primarily remembered as one of the seven cities mentioned in the book of Revelation. Because the city was in an earthquake-prone area, not much remains to be seen of ancient Philadelphia. What might still exist lies buried, for the most part, under the modern city. Situated approximately 30 miles southeast of the site of ancient Sardis on highway 585, Alaşehir is the name of the modern city located on the site of ancient Philadelphia. Philadelphia was on a plateau in the Cogamus River valley (today the Alaşehir Çayï), a tributary of the Hermus River. In antiquity, the Persian Royal Road from Sardis to Susa (in modern Iran) ran through Philadelphia. Prior to the Hellenistic founding of the city of Philadelphia, an earlier settlement here was known as Calletebus, dating back several centuries. The city was named for Attalus II Philadelphus, the Attalid king of Pergamum from 159 to 138 B.C.E., whose loyalty to his brother Eumenes II Soter, who preceded him as king (r. 197–159 B.C.E.), earned him the nickname “Philadelphus,” meaning “brotherly love.” Either Eumenes or Attalus founded the city, which was in the Lydian region of ancient Anatolia. After Attalus III (r. 138–133 B.C.E.) bequeathed the Pergamene kingdom to the Romans in 133 B.C.E., Philadelphia came under Roman control. The area around Philadelphia was a fertile agricultural area, especially good for growing grapes. Unfortunately, the area was also susceptible to frequent earthquakes. A particularly devastating earthquake struck the area in 17 C.E., destroying the city of Sardis and doing extensive damage to Philadelphia. To help the city recover from this disaster, Emperor Tiberius remitted the tribute owed to Rome for a period of five years. In gratitude, Philadelphia took the name Neocaesarea and dedicated a temple to Tiberius. Although the city was slow to recover from the devastation caused by the earthquake and its aftershocks, it eventually prospered under Roman rule. By the 5th century it was sometimes referred to as “little Athens” because of its many temples and religious festivals.

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