FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2080474021> ?p ?o ?g. }

• W2080474021 endingPage "242" @default.
• W2080474021 startingPage "233" @default.
• W2080474021 abstract "The Terlemez quartz monzonite is one of the Central Anatolian Granitoids and is exposed to the east of one of the main granitoid belts trending in a NW–SE direction and situated at the western end of the Central Anatolian Crystalline Complex. The Terlemez quartz monzonite is medium- to coarse-grained with granoblastic texture. It is essentially composed of quartz, plagioclase, hornblende and K-feldspar and variable contents of biotite. It is mostly compact and massive, but close to the contact with the ophiolitic basic rocks it shows a chilled margin. It characteristically includes K-feldspar megacrysts up to 3 cm in width and 10 cm in length, and contains irregular, angular or sub-rounded micromafic granular enclaves as well as xenoliths and large ‘roof-pendants’ of gabbroic composition derived from the Sarıkaraman Ophiolite, which is the most representative member of the supra-subduction zone type of Central Anatolian Ophiolites. The Terlemez quartz monzonite is a calc-alkaline, metaluminous intrusion. It typically displays moderately developed negative Ba and Nb trace element anomalies and enrichment in light rare earth elements relative to heavy rare earth elements without any significant Eu, Sr and Ti anomalies. On the basis of field, petrographic and geochemical data, the Terlemez quartz monzonite has been classified as H-type (hybrid type), which requires significant input from a mantle-derived mafic magma. The intrusion represents the advanced stage of the post-collisional magmatism of the Central Anatolian Crystalline Complex. Unlike the other Central Anatolian Granitoids, the Terlemez quartz monzonite has a clear intrusive contact with the well studied Middle Turonian–Lower Santonian Sarıkaraman Ophiolite. The K-Ar hornblende age obtained from the quartz monzonite (81·5 ± 1·9 Ma) is interpreted as the intrusion age. These data suggest a post-Early Santonian to pre-Early Campanian emplacement age for the supra-subduction zone type of Central Anatolian Ophiolites. The data further suggest that the post-collisional magmatism in Central Anatolia post-dates the emplacement of fore arc-type ophiolites onto the passive margin of the Tauride–Anatolide platform. The very short time interval between the formation and emplacement ages of supra-subduction zone-type ophiolites seems to be a very typical feature of the fore arc-type Eastern Mediterranean Ophiolites. Copyright © 1999 John Wiley & Sons, Ltd." @default.
• W2080474021 created "2016-06-24" @default.
• W2080474021 creator A5052354946 @default.
• W2080474021 creator A5060640853 @default.
• W2080474021 creator A5086970887 @default.
• W2080474021 creator A5089404412 @default.
• W2080474021 date "1999-07-01" @default.
• W2080474021 modified "2023-10-16" @default.
• W2080474021 title "Terlemez quartz monzonite of Central Anatolia (Aksaray-Sarıkaraman): age, petrogenesis and geotectonic implications for ophiolite emplacement" @default.
• W2080474021 cites W1970129893 @default.
• W2080474021 cites W1971477537 @default.
• W2080474021 cites W1971685925 @default.
• W2080474021 cites W1990305818 @default.
• W2080474021 cites W2021273178 @default.
• W2080474021 cites W2021987309 @default.
• W2080474021 cites W2044630803 @default.
• W2080474021 cites W2067988600 @default.
• W2080474021 cites W2069268089 @default.
• W2080474021 cites W2108971421 @default.
• W2080474021 cites W2117088195 @default.
• W2080474021 cites W2145604970 @default.
• W2080474021 cites W480060674 @default.
• W2080474021 doi "https://doi.org/10.1002/(sici)1099-1034(199907/09)34:3<233::aid-gj824>3.0.co;2-5" @default.
• W2080474021 hasPublicationYear "1999" @default.
• W2080474021 type Work @default.
• W2080474021 sameAs 2080474021 @default.
• W2080474021 citedByCount "54" @default.
• W2080474021 countsByYear W20804740212012 @default.
• W2080474021 countsByYear W20804740212013 @default.
• W2080474021 countsByYear W20804740212014 @default.
• W2080474021 countsByYear W20804740212016 @default.
• W2080474021 countsByYear W20804740212018 @default.
• W2080474021 countsByYear W20804740212019 @default.
• W2080474021 countsByYear W20804740212021 @default.
• W2080474021 countsByYear W20804740212022 @default.
• W2080474021 crossrefType "journal-article" @default.
• W2080474021 hasAuthorship W2080474021A5052354946 @default.
• W2080474021 hasAuthorship W2080474021A5060640853 @default.
• W2080474021 hasAuthorship W2080474021A5086970887 @default.
• W2080474021 hasAuthorship W2080474021A5089404412 @default.
• W2080474021 hasConcept C127313418 @default.
• W2080474021 hasConcept C151730666 @default.
• W2080474021 hasConcept C165205528 @default.
• W2080474021 hasConcept C167284885 @default.
• W2080474021 hasConcept C17409809 @default.
• W2080474021 hasConcept C20209278 @default.
• W2080474021 hasConcept C23923706 @default.
• W2080474021 hasConcept C2777229588 @default.
• W2080474021 hasConcept C2779181077 @default.
• W2080474021 hasConcept C2779870107 @default.
• W2080474021 hasConcept C34122518 @default.
• W2080474021 hasConcept C77928131 @default.
• W2080474021 hasConceptScore W2080474021C127313418 @default.
• W2080474021 hasConceptScore W2080474021C151730666 @default.
• W2080474021 hasConceptScore W2080474021C165205528 @default.
• W2080474021 hasConceptScore W2080474021C167284885 @default.
• W2080474021 hasConceptScore W2080474021C17409809 @default.
• W2080474021 hasConceptScore W2080474021C20209278 @default.
• W2080474021 hasConceptScore W2080474021C23923706 @default.
• W2080474021 hasConceptScore W2080474021C2777229588 @default.
• W2080474021 hasConceptScore W2080474021C2779181077 @default.
• W2080474021 hasConceptScore W2080474021C2779870107 @default.
• W2080474021 hasConceptScore W2080474021C34122518 @default.
• W2080474021 hasConceptScore W2080474021C77928131 @default.
• W2080474021 hasIssue "3" @default.
• W2080474021 hasLocation W20804740211 @default.
• W2080474021 hasOpenAccess W2080474021 @default.
• W2080474021 hasPrimaryLocation W20804740211 @default.
• W2080474021 hasRelatedWork W1951218480 @default.
• W2080474021 hasRelatedWork W1969139879 @default.
• W2080474021 hasRelatedWork W1973230640 @default.
• W2080474021 hasRelatedWork W2034057192 @default.
• W2080474021 hasRelatedWork W2053926192 @default.
• W2080474021 hasRelatedWork W2074216358 @default.
• W2080474021 hasRelatedWork W2549412327 @default.
• W2080474021 hasRelatedWork W2733480331 @default.
• W2080474021 hasRelatedWork W3128519641 @default.
• W2080474021 hasRelatedWork W2182773317 @default.
• W2080474021 hasVolume "34" @default.
• W2080474021 isParatext "false" @default.
• W2080474021 isRetracted "false" @default.
• W2080474021 magId "2080474021" @default.
• W2080474021 workType "article" @default.