Hydrocarbon reservoir depth identification in the eastern black sea basin: Implications from euler deconvolution and gravity tensor invariants

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Özet

The Black Sea Basin (BSB) consisting of Eastern Black Sea (EBS) and Western Black Sea (WBS) basins which separated by the Mid Black Sea High (MBSH) is formed by the collision of Eurasia and Arabian-African Plates. Petroleum and gas hydrate contents of the BSB have been discussed by using different geological and geophysical research. In this study, the gravity gradient tensor and invariant data based on the Bouguer gravity anomaly of the EBS basin were evaluated to define the hydrocarbon reservoirs. Afterwards, Euler deconvolution technique is applied to the invariant to reveal the depth of subsurface bodies. Furthermore, the significant invariant anomalies are compared with known oil seepage and petroleum wells. The depth values of oil trace closest to the known Sürmene and Hopa drill holes were computed as 4809 m, and 4455 m according to the structural index values of SI = 2.

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AlanDeğerDil
dc.contributor.authorDoğru, Fikret
dc.contributor.authorMaden, Nafiz
dc.date.accessioned2026-10-22T10:20:29.382810642Z
dc.date.available2026-10-22T10:20:29.382810642Z
dc.date.issued2023
dc.description.abstractThe Black Sea Basin (BSB) consisting of Eastern Black Sea (EBS) and Western Black Sea (WBS) basins which separated by the Mid Black Sea High (MBSH) is formed by the collision of Eurasia and Arabian-African Plates. Petroleum and gas hydrate contents of the BSB have been discussed by using different geological and geophysical research. In this study, the gravity gradient tensor and invariant data based on the Bouguer gravity anomaly of the EBS basin were evaluated to define the hydrocarbon reservoirs. Afterwards, Euler deconvolution technique is applied to the invariant to reveal the depth of subsurface bodies. Furthermore, the significant invariant anomalies are compared with known oil seepage and petroleum wells. The depth values of oil trace closest to the known Sürmene and Hopa drill holes were computed as 4809 m, and 4455 m according to the structural index values of SI = 2.
dc.identifier.articlenumber106201
dc.identifier.doi10.1016/j.marpetgeo.2023.106201
dc.identifier.eissn1873-4073
dc.identifier.issn0264-8172
dc.identifier.scopus2-s2.0-85149336730
dc.identifier.urihttps://rdlopen.rawdatalibrary.net/r/gumushane/12743
dc.identifier.volume151
dc.identifier.wosWOS:000949037500001
dc.language.isoen
dc.publisherElsevier Ltd
dc.relation.ispartofMarine and Petroleum Geology
dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectBlack sea
dc.subjectEuler deconvolution
dc.subjectGravity
dc.subjectInvariant
dc.subjectTensor
dc.subject.classificationGeosciences, Multidisciplinary
dc.subject.classificationGeology
dc.subject.otherBlack Sea
dc.subject.otherGas hydrates
dc.subject.otherGasoline
dc.subject.otherGravitation
dc.subject.otherHydrocarbons
dc.subject.otherSeepage
dc.subject.otherBouguer gravity anomalies
dc.subject.otherEuler deconvolution
dc.subject.otherEurasia
dc.subject.otherGeological research
dc.subject.otherGeophysical researches
dc.subject.otherGravity gradient tensors
dc.subject.otherHydrocarbon reservoir
dc.subject.otherInvariant
dc.subject.otherTensor invariants
dc.subject.otherAfrican plate
dc.subject.otherArabian plate
dc.subject.otherdeconvolution
dc.subject.otherEurasian plate
dc.subject.othergas hydrate
dc.subject.othergravity anomaly
dc.subject.otherocean basin
dc.subject.otheroil seep
dc.subject.otherpetroleum
dc.subject.otherTensors
dc.titleHydrocarbon reservoir depth identification in the eastern black sea basin: Implications from euler deconvolution and gravity tensor invariants
dc.typeArticle
dspace.entity.typePublication
rdl.citation.openalex5
rdl.citation.scopus4
rdl.citation.wos4
rdl.oa.statusclosed
rdl.source.indexSCOPUS
rdl.source.indexWOS
rdl.wos.indexScience Citation Index Expanded (SCI-EXPANDED)