FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2097080189> ?p ?o ?g. }

• W2097080189 abstract "The North Anatolian fault is a 1200-km-long major transform fault bounding the Anatolian plate on its north side. The fault formed during the late middle Miocene as a broad shear zone with a number of strands splaying westward in a horsetail pattern. Later, movement became localized along a central strand, and the southerly and northerly splays became inactive. The west-northwest-striking Thrace strike-slip fault system is one of these right-lateral, presently inactive, splays. It consists of three subparallel strike-slip faults. From north to south these are the Kirklareli, Luleburgaz, and Babaeski fault zones, which extend for about 130 km through the Thrace basin. The Thrace fault zone probably connected to the southeast with the presently active northern strand of the North Anatolian fault in the Marmara Sea. To the northwest, the zone may have extended to the Plovdiv graben zone in Bulgaria. The Cenozoic Thrace basin contains middle Eocene to Pliocene sedimentary rocks. The Thrace right-lateral wrench fault system formed prior to the Pliocene and had become inactive by the Pliocene. Strike-slip fault zones with normal and reverse separation are detected by seismic reflection profiles and subsurface data. As the system became inactive, the motion on the North Anatolian fault zone began to be accommodated in the Marmara Sea region. Thus, the Thrace fault system represents the oldest strand of the North Anatolian fault to the west of Istanbul. Releasing-bend extensional structures and restraining-bend compressional structures are abundant along the fault zones. Several hydrocarbon-producing anticlines lie en echelon to the Luleburgaz fault zone. Regionally, the Thrace fault ystem has a horsetail shape, with the various strands becoming younger southward." @default.
• W2097080189 created "2016-06-24" @default.
• W2097080189 creator A5025889975 @default.
• W2097080189 date "1991-01-01" @default.
• W2097080189 modified "2023-10-12" @default.
• W2097080189 title "Possible Strand of the North Anatolian Fault in the Thrace Basin, Turkey--An Interpretation (1)" @default.
• W2097080189 cites W1550272795 @default.
• W2097080189 cites W1569360278 @default.
• W2097080189 cites W1986005980 @default.
• W2097080189 cites W1994419673 @default.
• W2097080189 cites W2004955914 @default.
• W2097080189 cites W2021176165 @default.
• W2097080189 cites W2045594539 @default.
• W2097080189 cites W2073951015 @default.
• W2097080189 cites W2074721947 @default.
• W2097080189 cites W2084476899 @default.
• W2097080189 cites W2136183843 @default.
• W2097080189 cites W2153210255 @default.
• W2097080189 cites W2153833792 @default.
• W2097080189 cites W2171737953 @default.
• W2097080189 cites W2326169835 @default.
• W2097080189 cites W2329323373 @default.
• W2097080189 cites W2332174487 @default.
• W2097080189 cites W644712492 @default.
• W2097080189 doi "https://doi.org/10.1306/0c9b2795-1710-11d7-8645000102c1865d" @default.
• W2097080189 hasPublicationYear "1991" @default.
• W2097080189 type Work @default.
• W2097080189 sameAs 2097080189 @default.
• W2097080189 citedByCount "24" @default.
• W2097080189 countsByYear W20970801892012 @default.
• W2097080189 countsByYear W20970801892015 @default.
• W2097080189 countsByYear W20970801892017 @default.
• W2097080189 countsByYear W20970801892018 @default.
• W2097080189 countsByYear W20970801892020 @default.
• W2097080189 countsByYear W20970801892022 @default.
• W2097080189 countsByYear W20970801892023 @default.
• W2097080189 crossrefType "journal-article" @default.
• W2097080189 hasAuthorship W2097080189A5025889975 @default.
• W2097080189 hasConcept C109007969 @default.
• W2097080189 hasConcept C127313418 @default.
• W2097080189 hasConcept C151730666 @default.
• W2097080189 hasConcept C165205528 @default.
• W2097080189 hasConcept C16674752 @default.
• W2097080189 hasConcept C17409809 @default.
• W2097080189 hasConcept C175551986 @default.
• W2097080189 hasConcept C199360897 @default.
• W2097080189 hasConcept C2778958684 @default.
• W2097080189 hasConcept C41008148 @default.
• W2097080189 hasConcept C527412718 @default.
• W2097080189 hasConceptScore W2097080189C109007969 @default.
• W2097080189 hasConceptScore W2097080189C127313418 @default.
• W2097080189 hasConceptScore W2097080189C151730666 @default.
• W2097080189 hasConceptScore W2097080189C165205528 @default.
• W2097080189 hasConceptScore W2097080189C16674752 @default.
• W2097080189 hasConceptScore W2097080189C17409809 @default.
• W2097080189 hasConceptScore W2097080189C175551986 @default.
• W2097080189 hasConceptScore W2097080189C199360897 @default.
• W2097080189 hasConceptScore W2097080189C2778958684 @default.
• W2097080189 hasConceptScore W2097080189C41008148 @default.
• W2097080189 hasConceptScore W2097080189C527412718 @default.
• W2097080189 hasLocation W20970801891 @default.
• W2097080189 hasOpenAccess W2097080189 @default.
• W2097080189 hasPrimaryLocation W20970801891 @default.
• W2097080189 hasRelatedWork W1547281 @default.
• W2097080189 hasRelatedWork W1978330345 @default.
• W2097080189 hasRelatedWork W2044967351 @default.
• W2097080189 hasRelatedWork W2104696163 @default.
• W2097080189 hasRelatedWork W2128877651 @default.
• W2097080189 hasRelatedWork W2325222095 @default.
• W2097080189 hasRelatedWork W2347388628 @default.
• W2097080189 hasRelatedWork W2355033796 @default.
• W2097080189 hasRelatedWork W2356014781 @default.
• W2097080189 hasRelatedWork W4240162436 @default.
• W2097080189 hasVolume "75" @default.
• W2097080189 isParatext "false" @default.
• W2097080189 isRetracted "false" @default.
• W2097080189 magId "2097080189" @default.
• W2097080189 workType "article" @default.