Srpenica seismites - indicators of paleoseismicity in the Upper Soča valley, NW Slovenia

Authors

  • Tihomir Marjanac
  • Ljerka Marjanac
  • Marijan Poljak
  • Mladen Živčič
  • Miloš Bavec

DOI:

https://doi.org/10.5474/geologija.2001.026

Abstract

Varve-like lacustrine sediments of Pleistocene to Holocene age were studied in the abandoned clay pit near Srpenica in the Upper Soča valley. Within a sequence of laminated to thin bedded lacustrine deposits, two intervals of soft-sediment deformations were studied and interpreted herein in terms of seismites. The age of deformation is estimated by a radiocarbon date of wood (at the top of the lower deformed layer) at 12790±85 14C years BP, and the genesis is attributed to strong past earthquakes, which is very much in accordance with the present seismicity of the studied area.

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How to Cite

Marjanac, T., Marjanac, L., Poljak, M., Živčič, M., & Bavec, M. (2001). Srpenica seismites - indicators of paleoseismicity in the Upper Soča valley, NW Slovenia . Geologija, 44(2), 341–350. https://doi.org/10.5474/geologija.2001.026

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