The origin and P-T conditions of the metamorphic sole rocks beneath the Late Cretaceous Pınarbaşı Ophiolite, Eastern-Central Anatolia
Author:
Affiliation:
1. Kocaeli Üniversitesi Jeoloji Mühendisliği Bölümü, Kocaeli, 41380, Türkiye
2. Dipartimento Territorio e dei Sistemi Agro-Forestali, Università di Padova, 35020-Legnaro, Italy
Funder
Kocaeli Üniversitesi
Türkiye Bilimsel ve Teknolojik Arastirma Kurumu
Publisher
Informa UK Limited
Subject
Geology
Link
https://www.tandfonline.com/doi/pdf/10.1080/00206814.2022.2045638
Reference99 articles.
1. Plate interface rheological switches during subduction infancy: Control on slab penetration and metamorphic sole formation
2. Osmium isotope systematics and highly siderophile element fractionation in spinel-peridotites from the Tethyan ophiolites in SW Turkey: Implications for multi-stage evolution of oceanic upper mantle
3. Geochemical character and tectonic environment of ultramafic to mafic cumulate rocks from the Tekirova (Antalya) ophiolite (southern Turkey)
4. Geochemical discrimination between ocean-floor and island-arc tholeiites—application to some ophiolites
5. Structure and metamorphism of a subducted seamount (Zagros suture, Southern Iran)
Cited by 1 articles. 订阅此论文施引文献 订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献
1. Early–Middle Jurassic metamorphic and non-metamorphic supra-subduction zone ophiolite fragments in a Late Cretaceous ophiolitic mélange (northern Turkey): implications for long-lived and supra-subduction zone ophiolite formation;International Journal of Earth Sciences;2022-08-12
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