Seismogenic structures in Quaternary lacustrine deposits of Lake Van (eastern Turkey)
Soft-sediment deformation structures formed by liquefaction and/or fluidisation of unconsolidated sediments due to seismic shocks are frequent in the Quaternary sandy, silty and clayey deposits of Lake Van. They are present in both marginal and deep lacustrine facies. Their morphology and interprete...
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| Format: | Article |
| Language: | English |
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Sciendo
2014-07-01
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| Series: | Geologos |
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| Online Access: | https://doi.org/10.2478/logos-2014-0011 |