Factors affecting thickness and frequency of turbidites triggered by earthquakes in Kumburgaz Basin, Sea of Marmara

Submerged fault ruptures generate earthquake-triggered mass flow deposits, which are extensively used as a tool in subaqueous paleoseismology. In tectonically active deep sedimentary basins, such as the Sea of Marmara (SoM), these mass flow deposits are defined as turbidite-homogenite units (THUs),...

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Veröffentlicht in:Marine geology 2022-10, Vol.452, p.106900, Article 106900
Hauptverfasser: Yakupoğlu, Nurettin, Henry, Pierre, Uçarkuş, Gülsen, Eriş, K. Kadir, Demory, François, Crouzet, Christian, Çağatay, M. Namık
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Sprache:eng
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