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- W2184902991 abstract "Naxos is part of the exhumed metamorphic belt in the Aegean Sea and features a distinguished geology, comprising structural records of at least Eocene-present tectonic events on a broad variety of scales. Meso-scaled structures as the Naxos-Paros extensional fault systems and the metamorphic core complex on Naxos reveal a complicated history of extensional tectonics in the back-arc basin that has led to the exhumation of high-grade metamorphic rocks, juxtaposing them against significantly younger material of Miocene age. The exact driving mechanisms for the MCC uplift are still debated, but recent research indicates that the MMC’s uplift was caused by a combination of buoyancy- and isostasy-driven flow during phases of Barrovian metamorphism in an extensional regime, with upper-plate-to-the-north sense of shear." @default.
- W2184902991 created "2016-06-24" @default.
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- W2184902991 date "2014-01-01" @default.
- W2184902991 modified "2023-09-27" @default.
- W2184902991 title "DETACHMENT FAULTING AND THE METAMORPHIC CORE COMPLEX ON NAXOS, GREECE" @default.
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