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akaturk Akademik ölçüm

Makale detayı · 2002

The role of the flexural rotation rolling hinge model in the tectonic evolution of the Alasehir graben western Turkey

Dergi

Geological Magazine

ISSN 0016-7568

YÖKSİS OpenAlex SJR Q1 JCR Q1 Atıf 135 Üst %10 Yüzdelik 98.3% FWCI 7.83
Yıl
2002
Tür
article

Veri kaynağı ayrımı

  • YÖKSİS YÖKSİS makale kaydı
  • YÖKSİS dergi adı Geological Magazine
  • Katalog eşleşmesi (ISSN) Geological Magazine
  • OpenAlex OpenAlex zenginleştirmesi (özet, atıf, konular)

Özet

OpenAlex · İngilizce

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.

Konular

Atıflar

OpenAlex cited_by_count. WoS veya Scopus atıf sayısı değildir; o kaynaklar için ayrı kolon yoktur.

135 atıf

OpenAlex cited_by_count (önbellek / veritabanı)

Yerel katalogda bu makaleye atıf yapan 82 yayın (OpenAlex referans eşleşmesi; tam dünya listesi değildir).

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  2. Origin of NE-trending basins in western Turkey 2003 Atıf 246 · OpenAlex
  3. Ductile brittle transition along the Alaşehir detachment fault and its structural relationship with the Simav detachment fault Menderes massif western Turkey 2003 Atıf 151 · OpenAlex
  4. Ductile brittle transition along the Alaşehir detachment fault and its structural relationship with the Simav detachment fault Menderes massif western Turkey 2003 Atıf 150 · OpenAlex
  5. The 40Ar 39Ar age of extensional ductile deformation and granitoid intrusion in the northern Menderes core complex implications for the initiation of extensional tectonics in western Turkey 2004 Atıf 140 · OpenAlex
  6. Complete Tertiary exhumation history of the Menderes massif western Turkey an alternative working hypothesis 2004 Atıf 132 · OpenAlex
  7. Complete Tertiary exhumation history of the Menderes massif western Turkey an alternative working hypothesis 2004 Atıf 132 · OpenAlex
  8. Sedimentary facies depositional environments and palaeogeographicevolution of the Neogene Denizli Basin SW Anatolia Turkey 2007 Atıf 131 · OpenAlex
  9. From palaeotectonics to neotectonics in the Neotethys realm Theimportance of kinematic decoupling and inherited structural grain in SWAnatolia Turkey 2009 Atıf 126 · OpenAlex
  10. Tectonic implications of transtensional supradetachment basin development in an extension parallel transfer zone the Kocaçay Basin western Anatolia Turkey 2011 Atıf 105 · OpenAlex

Yazarlar

  1. GÜROL SEYİTOĞLU
  2. Okan Tekeli
  3. Ibrahim Cemen
  4. Şevket Şen
  5. VEYSEL IŞIK ANKARA ÜNİVERSİTESİ