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Article detail · 2023

Tectonic geomorphology of Bozdoğan and Karacasu grabens, western Anatolia

Journal

Geologica Acta

ISSN 1695-6133

YÖKSİS OpenAlex Open access · diamond SJR Q2 JCR Q2 Citations 8 Percentile 77.5% FWCI 1.48
Year
2023
Type
article

Data source split

  • YÖKSİS YÖKSİS article record
  • YÖKSİS venue Geologica Acta
  • Catalog match (ISSN) Geologica Acta
  • OpenAlex OpenAlex enrichment (abstract, citations, topics)

Abstract

OpenAlex · English

Western Anatolia is one of the most rapidly extending and seismically active regions in the world. The circa N-S extension since the Early Miocene caused the formation of E-W trending major grabens and intervening horsts, having earthquake potentials with magnitude ≥5. The E-W oriented Büyük Menderes graben cross-cuts the broadly N-S oriented Bozdoğan and Karacasu grabens, of which the boundary faults of the latter are the source of seismic activity. Geomorphic indices, including drainage basin asymmetry, mountain front sinuosity, valley-floor width to valley height ratio, stream length-gradient index and normalized channel steepness index, were used to evaluate the boundary fault segments of the Bozdoğan and Karacasu grabens. The results indicate that both grabens are tectonically active and therefore regions of earthquake potential, consistent with the epicenters of earthquakes. Thus, it can be inferred that fault segments of second-order grabens, which are crosscut by the boundary faults of seismically active main depressions, are apparently reactivated by ongoing tectonism and may represent seismic activity. This suggestion applies also for similar basins located in the western Anatolia.

Topics

Citations

OpenAlex cited_by_count. Not a WoS or Scopus citation count; those sources have no separate column here.

8 citations

OpenAlex cited_by_count (cache / database)

Authors

  1. ERMAN ÖZSAYIN
  2. Kadir Kırık
  3. FARUK OCAKOĞLU
  4. AZAD SAĞLAM SELÇUK VAN YÜZÜNCÜ YIL ÜNİVERSİTESİ