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

Abstract

The 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

Distribution of rocks in Pınarbaşı Ophiolite from central Anatolia (Turkey) based on analysis of ASTER and Landsat‐8 data

“…Ophiolites, which are parts of the oceanic lithosphere, contain a wide range of lithologies such as peridotites, gabbros, and basalts and can be observed on the continents and in the accretionary complexes of suture zones (e.g., Çelik, Chiaradia, Marzoli, Billor, & Marschik, 2013; Çelik et al, 2019; Coleman, 1984; Dilek & Furnes, 2009; Moores, 1982; Nicolas, 1989; Steinmann, 1927; Yang et al, 2019). Mapping of ophiolites and accretionary complexes reveals: (a) the plate tectonic history and the emplacement of former oceanic basins (e.g., Çelik et al, 2013, 2016; Çörtük et al, 2016; Göçmengil, Altıntaş, Topuz, Çelik, & Özkan, 2013; Özkan, Çelik, Soycan, Çörtük, & Marzoli, 2020; Topuz et al, 2013), (b) distribution of mantle and crustal rocks of the oceanic lithosphere, and (c) the spatial distribution of associated economic deposits of ore minerals (e.g., chromite, manganese; Aldanmaz, Meisel, Celik, & Henjes‐Kunst, 2012; Çelik et al, 2013, 2016; Çörtük et al, 2016).…”