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dc.contributor.authorYalamaz, Burak
dc.contributor.authorCagatay, M.Namik
dc.contributor.authorBulkan, Özlem
dc.date.accessioned2025-03-08T01:08:39Z
dc.date.available2025-03-08T01:08:39Z
dc.date.issued2020
dc.date.submitted2022-06-01T12:12:36Z
dc.identifierONIX_20220601_9788855181471_245
dc.identifier2704-5846
dc.identifierhttps://library.oapen.org/handle/20.500.12657/56062
dc.identifier.urihttps://doab-dev.siscern.org/handle/20.500.12854/173811
dc.description.abstractThis study represents the lithological correlation of multi-cores taken from the various parts of the current Lake Bafa basin, BAF35, - 37 - 39 - 41, - 42, - 46. Concerning the main depositional characteristics, we reconstructed fundamental characteristics of local abrupt and gradual environmental fluctuations. The gradual changes reflect four main environmental phases are lacustrine stage (last 0.8 ky), lagoon stage (0.8–1.75 ky BP), marine-river interaction stage (1.75–2.7 ky BP) and the earliest marine-dominated stage (>2.7 ky BP).
dc.languageEnglish
dc.relation.ispartofseriesProceedings e report
dc.rightsopen access
dc.subject.otherTransitional environment
dc.subject.otherMediterranean Sea Coast
dc.subject.otherLacustrine
dc.subject.otherSedimentology
dc.subject.otherPaleolimnology
dc.titleChapter A sedimentological pattern of a coastal transitional environment: from the Eastern Mediterranean Sea shoreline through the Lake Bafa
dc.typechapter
oapen.identifier.doi10.36253/978-88-5518-147-1.38
oapen.relation.isPublishedBy2ec4474d-93b1-4cfa-b313-9c6019b51b1a
oapen.relation.isbn9788855181471
oapen.pages7
oapen.place.publicationFlorence
dc.seriesnumber126


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