@ARTICLE{Ubeid_Khalid_Fathi_Tsunami_2021,
 author={Ubeid, Khalid Fathi},
 volume={vol. 38},
 number={No 1},
 journal={Studia Quaternaria},
 pages={43-51},
 howpublished={online},
 year={2021},
 publisher={Committee for Quaternary Research PAS},
 publisher={Institute of Geological Sciences PAS},
 abstract={The outcrop of the tsunami deposits, about 6 m thick, is located in the archaeological site Tel Askan in the Al Zhraa locality, southwest of the Gaza City. These deposits are unconformably underlain by sand dunes and sharply overlain by a palaeosol. They are pale gray sands mixed with volcanic ash and fine-grained deposits, and are intercalated with peat, few centimetres thick. The sand-sized grains are well rounded and well sorted, and consist mainly of quartz and subordinate of feldspar. Both macro- and microfossils were observed from tsunami deposits. Additionally, rip-up clasts and pottery shards were observed, indicating higher-flow regime. The potteries in tsunami deposits provide evidence for tsunami inundation at distance of about 1 km from the present shoreline.},
 type={Article},
 title={Tsunami event identified in a sedimentary record of the Gaza Strip, Palestine},
 URL={http://www.czasopisma.pan.pl/Content/119628/4_Ubeid.pdf},
 doi={10.24425/sq.2021.136823},
 keywords={tsunami, sedimentology, pottery shard, rip-up clast, Gaza Strip},
}