Dergi makalesi Açık Erişim
GORUR, N; TUYSUZ, O; AYKOL, A; SAKINC, M; YIGITBAS, E; AKKOK, R
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<identifier identifierType="URL">https://aperta.ulakbim.gov.tr/record/101711</identifier>
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<creatorName>GORUR, N</creatorName>
<givenName>N</givenName>
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<creator>
<creatorName>TUYSUZ, O</creatorName>
<givenName>O</givenName>
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<creator>
<creatorName>AYKOL, A</creatorName>
<givenName>A</givenName>
<familyName>AYKOL</familyName>
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<creator>
<creatorName>SAKINC, M</creatorName>
<givenName>M</givenName>
<familyName>SAKINC</familyName>
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<creator>
<creatorName>YIGITBAS, E</creatorName>
<givenName>E</givenName>
<familyName>YIGITBAS</familyName>
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<creator>
<creatorName>AKKOK, R</creatorName>
<givenName>R</givenName>
<familyName>AKKOK</familyName>
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<titles>
<title>Cretaceous Red Pelagic Carbonates Of Northern Turkey - Their Place In The Opening History Of The Black-Sea</title>
</titles>
<publisher>Aperta</publisher>
<publicationYear>1993</publicationYear>
<dates>
<date dateType="Issued">1993-01-01</date>
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<resourceType resourceTypeGeneral="Text">Journal article</resourceType>
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<alternateIdentifier alternateIdentifierType="url">https://aperta.ulakbim.gov.tr/record/101711</alternateIdentifier>
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<relatedIdentifier relatedIdentifierType="DOI" relationType="IsVersionOf">10.81043/aperta.101710</relatedIdentifier>
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<rights rightsURI="http://www.opendefinition.org/licenses/cc-by">Creative Commons Attribution</rights>
<rights rightsURI="info:eu-repo/semantics/openAccess">Open Access</rights>
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<descriptions>
<description descriptionType="Abstract">Northern Turkey forms a part of the Rhodope-Pontide Fragment, one of Turkey's main tectono-stratigraphic units. Cretaceous geology of this region is characterized by the presence of a series of horsts, grabens and tilted and rotated fault blocks buried beneath the Upper Cretaceous to Lower Tertiary volcanic material-bearing turbiditic sediments. These structures and sedimentary and igneous rocks represent the most complete record of the opening of the oceanic Black Sea back-arc basin which began forming in the Aptian-Albian behind a continental extensional margin magmatic arc. This was followed by a fault-controlled syn-rift sedimentation and subsidence until the late Cenomanain when sea-floor spreading in the basin and thermally-induced subsidence of the basin margins started.</description>
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