2018
DOI: 10.1016/j.lithos.2017.12.025
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Latest Cretaceous “A2-type” granites in the Sakarya Zone, NE Turkey: Partial melting of mafic lower crust in response to roll-back of Neo-Tethyan oceanic lithosphere

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Cited by 53 publications
(13 citation statements)
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“…Our slab rollback model appears to be reasonable at explaining the spatial and temporal variation and compositional transition of the Late Cretaceous magmatism, as well as the presence of the approximately 81‐ to 73‐Ma A 2 ‐type alkaline granitoids with high zircon saturation temperatures (up to 862 °C) in the Pirnalli and Topcam area of the EP (Figure b, Karsli et al, ; Karsli, Caran, et al, ). However, we note that the validity of this model is subject to future work using the data of the coeval mafic rocks and the abundant geochronological data of the Late Cretaceous magmatism in the EP arc.…”
Section: Discussionsupporting
confidence: 56%
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“…Our slab rollback model appears to be reasonable at explaining the spatial and temporal variation and compositional transition of the Late Cretaceous magmatism, as well as the presence of the approximately 81‐ to 73‐Ma A 2 ‐type alkaline granitoids with high zircon saturation temperatures (up to 862 °C) in the Pirnalli and Topcam area of the EP (Figure b, Karsli et al, ; Karsli, Caran, et al, ). However, we note that the validity of this model is subject to future work using the data of the coeval mafic rocks and the abundant geochronological data of the Late Cretaceous magmatism in the EP arc.…”
Section: Discussionsupporting
confidence: 56%
“…We note that a slab rollback model associated with the northward subduction of the northern branch of the Neotethys lithosphere has also been proposed to explain the generation of the Late Cretaceous magmatic rocks both in the EP (e.g., Çinku et al, ; Karsli et al, ; Karsli, Caran, et al, ) and the western Pontides (e.g., Aysal et al, ; Keskin & Tüysüz, ) on the basis of an assumed southward migration of magmatism that was inferred from the paleomagnetic data (Çinku et al, ). However, as discussed earlier, existing data indicate that the Late Cretaceous magmatism did not show a simple southward migration but covers a broader region not only in the northern zone (Ordu‐Güdül) but also in the southern zone (Gümüşhane‐Bayburt) of the EP (Figure b).…”
Section: Discussionmentioning
confidence: 81%
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