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Blueschist facies overprint of late Triassic Tethyan oceanic crust in a subduction–accretion complex in north-central Anatolia, Turkey

dc.contributor.authorÇelik, Ömer Faruk
dc.contributor.authorÖzkan, Mutlu
dc.contributor.authorChelle-Michou, Cyril
dc.contributor.authorSherlock, Sarah
dc.contributor.authorMarzoli, Andrea
dc.contributor.authorUlianov, Alexey
dc.contributor.authorAltıntaş, İsmail Emir
dc.contributor.authorTopuz, Gültekin
dc.date.accessioned2026-01-26T04:07:50Z
dc.date.issued2018-10-22
dc.description.abstractThe late Cretaceous accretionary complex along the İzmir–Ankara–Erzincan suture zone, northern Turkey, includes various types of metamorphic rock together with radiolarite, sandstone, mudstone, serpentinite, basalt and limestone. Meta-plagiogranite blocks (up to 5 m in diameter) and a meta-gabbro slice (800 × 500 m) cross-cut by meta-plagiogranite are observed in a matrix of serpentinite, mudstone and radiolarian chert. These meta-gabbros and meta-plagiogranites show subduction-related geochemical characteristics. Laser ablation inductively coupled plasma mass spectrometry U–Pb dating of zircons from two meta-plagiogranites yielded 222.3 ± 1.5 and 227.2 ± 1.6 Ma crystallization ages. This study shows that the meta-gabbro and meta-plagiogranite from the accretionary complex are remnants of the metamorphosed equivalents of the late Triassic lower crustal rocks of the subducted Tethyan oceanic crust. They are the oldest lower crustal rocks observed in the İzmir–Ankara–Erzincan suture zone. Both the meta-gabbros and meta-plagiogranites have Na–Ca amphiboles, indicating blueschist facies metamorphism. However, phengites from a blueschist facies rock yielded an 40 Ar/ 39 Ar age of 104.3 ± 0.7 Ma, indicating that blueschist metamorphism occurred during the Albian. All these data suggest that the oceanic crust formed during the Norian, metamorphosed during the Jurassic to early Cretaceous and then dismembered during accretionary complex formation in the late Cretaceous. Supplementary material: A complete description of the analytical methods ( electron microprobe, LA-ICP-MS zircon U–Pb and 40 Ar/ 39 Ar age analyses, pseudo-section modelling and THERMOCALC) are available at https://doi.org/10.6084/m9.figshare.6509984 Thematic collection: This article is part of the ‘Tethyan ophiolites and Tethyan seaways collection’ available at: https://www.lyellcollection.org/cc/tethyan-ophiolites-and-tethyan-seaways
dc.description.urihttps://doi.org/10.1144/jgs2018-045
dc.description.urihttps://dx.doi.org/10.1144/jgs2018-045
dc.description.urihttps://avesis.kocaeli.edu.tr/publication/details/103185ef-d388-4187-b322-3fadb5c92940/oai
dc.description.urihttps://hdl.handle.net/11577/3455578
dc.description.urihttps://aperta.ulakbim.gov.tr/record/70183
dc.identifier.doi10.1144/jgs2018-045
dc.identifier.eissn2041-479X
dc.identifier.endpage957
dc.identifier.issn0016-7649
dc.identifier.openairedoi_dedup___::db5014b95f2d82f92b2e062486d6f0a9
dc.identifier.orcid0000-0003-2369-4810
dc.identifier.orcid0000-0002-9948-488x
dc.identifier.orcid0000-0003-1760-3492
dc.identifier.orcid0000-0003-0494-6760
dc.identifier.orcid0000-0003-0093-2759
dc.identifier.startpage945
dc.identifier.urihttps://hdl.handle.net/11527/60159
dc.identifier.volume176
dc.language.isoeng
dc.publisherGeological Society of London
dc.relation.ispartofJournal of the Geological Society
dc.rightsOPEN
dc.sdg.typeGoal 13: Climate Action
dc.sdg.typeGoal 15: Life on Land
dc.titleBlueschist facies overprint of late Triassic Tethyan oceanic crust in a subduction–accretion complex in north-central Anatolia, Turkey
dc.typeArticle
dspace.entity.typePublication

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