Selcuk, LeventCiftci, Yahya2025-05-102025-05-1020071435-952910.1007/s10064-006-0052-32-s2.0-34247637408https://doi.org/10.1007/s10064-006-0052-3https://hdl.handle.net/20.500.14720/12510Selcuk, Levent/0000-0002-7060-8260Yuzuncu University (YYU) campus area is located on the eastern shore of Lake Van, within one of the active tectonic belts of Eastern Anatolia. The sediments accumulated in a lake formed when the Murat River was dammed by volcanoclastic deposits and hence include lacustrine, fluvial and sandy shore sediments. In order to delineate the liquefaction-prone soils, geological and geophysical data were assessed. On the basis of the Liquefaction Potential Index (I-L), three main geotechnical zones were identified in the study area and three microzones were delineated within the university campus to reflection the potential damage to structures.eninfo:eu-repo/semantics/closedAccessLiquefactionPlio-Quaternary LacustrineFluviatile DepositsMicrozonationLake Van BasinTurkeyArticle662Q1Q1161176WOS:000246094600005