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Geological evolution of the Gulf of Saros, NE Aegean Sea

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dc.contributor.authorÇağatay, M. N.
dc.contributor.authorGörür, N.
dc.contributor.authorAlpar, B.
dc.contributor.authorSaatçılar, R.
dc.contributor.authorAkkök, R.
dc.contributor.authorSakınç, M.
dc.contributor.authorYüce, H.
dc.contributor.authorYaltırak, C.
dc.contributor.authorKuşcu, I.
dc.date.accessioned2026-01-25T05:32:33Z
dc.date.issued1998-05-11
dc.description.abstractThe Gulf of Saros is an Upper Miocene transtensional basin in NW Anatolia, formed by the interaction between the North Anatolian Fault and the N-S extensional tectonic regime of the Aegean. The present configuration of the basin evolved mainly during the Plio-Quaternary under the increased activity of the North Anatolian Fault. During the late Miocene-late Quaternary, no sedimentation took place on the shelves. After this long hiatus, an important change in tectonic style about 0.2 Ma BP allowed sedimentation to resume in the gulf.
dc.description.urihttps://doi.org/10.1007/s003670050045
dc.description.urihttps://dx.doi.org/10.1007/s003670050045
dc.identifier.doi10.1007/s003670050045
dc.identifier.eissn1432-1157
dc.identifier.endpage9
dc.identifier.issn0276-0460
dc.identifier.openairedoi_dedup___::6d64b7db6b83f7412696599f97dd8889
dc.identifier.orcid0000-0002-9694-1395
dc.identifier.startpage1
dc.identifier.urihttps://hdl.handle.net/11527/47052
dc.identifier.volume18
dc.publisherSpringer Science and Business Media LLC
dc.relation.ispartofGeo-Marine Letters
dc.rightsCLOSED
dc.sdg.typeGoal 13: Climate Action
dc.sdg.typeGoal 14: Life Below Water
dc.titleGeological evolution of the Gulf of Saros, NE Aegean Sea
dc.typeArticle
dspace.entity.typePublication

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