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S Acikalin

Biographic Data

ID6571378
NAMES Acikalin
GIVEN NAMESS
FAMILY NAMEAcikalin
SIGNATUREACIKALIN S
AFFILIATIONSEskişehir Osmangazi University, Department of Geological Engineering, Eskişehir, Turkey
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS1
AUTHOR COUNT1
EDITOR COUNT0
FIRST PUBLICATION YEAR2009
LATEST PUBLICATION YEAR2009
H-INDEX1
  • A multistory gigantic subaerial debris flow in an active fault scarp in NW Anatolia, Turkey

    Open Access•Faruk Ocakoğlu, S Acikalin et al.•ARTICLE•The Holocene•2009•Cited by: 1•References: 3

    Mass instability in the uplifting footwall blocks of normal faults involves a range of regional and local factors including, among others, climatic setting, topography, lithology and particularly ground shaking during earthquakes. Morphological and sedimentological investigations backed by 14 C dating on a huge debris flow and its zone of depreciation provided favorable insights for dynamics and causative factors of this mass wasting. Our observa…

  • A multistory gigantic subaerial debris flow in an active fault scarp in NW Anatolia, Turkey

    Open Access•Faruk Ocakoğlu, S Acikalin et al.•ARTICLE•The Holocene•2009•Cited by: 1•References: 3

    Mass instability in the uplifting footwall blocks of normal faults involves a range of regional and local factors including, among others, climatic setting, topography, lithology and particularly ground shaking during earthquakes. Morphological and sedimentological investigations backed by 14 C dating on a huge debris flow and its zone of depreciation provided favorable insights for dynamics and causative factors of this mass wasting. Our observa…

  • A multistory gigantic subaerial debris flow in an active fault scarp in NW Anatolia, Turkey

    Open Access•Faruk Ocakoğlu, S Acikalin et al.•ARTICLE•The Holocene•2009•Cited by: 1•References: 3

    Mass instability in the uplifting footwall blocks of normal faults involves a range of regional and local factors including, among others, climatic setting, topography, lithology and particularly ground shaking during earthquakes. Morphological and sedimentological investigations backed by 14 C dating on a huge debris flow and its zone of depreciation provided favorable insights for dynamics and causative factors of this mass wasting. Our observa…

Debris (1 works) · Debris flow (1 works) · earthquake and tectonic studies (1 works) · Fault (geology (1 works) · Fault scarp (1 works) · Geology (1 works) · Geology and Paleoclimatology Research (1 works) · Geomorphology (1 works) · Holocene (1 works) · Landslide (1 works)

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