Jurassic to early Cretaceous geodynamic evolution of the eastern Hellenides
Remarkably well-preserved crustal sections from the Eastern Hellenides offer the chance to evaluate the regional geodynamic evolution of continental crust. Here, we identify and geodynamically interpret eclogite facies metamorphism in the Triassic–Jurassic volcano-sedimentary series of the West Circ...
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| Veröffentlicht in: | International journal of earth sciences : Geologische Rundschau 2024-02, Vol.113 (1), p.1-22 |
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| container_title | International journal of earth sciences : Geologische Rundschau |
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| creator | Mposkos, Evripidis Krohe, Alexander Walton, Craig Baziotis, Ioannis |
| description | Remarkably well-preserved crustal sections from the Eastern Hellenides offer the chance to evaluate the regional geodynamic evolution of continental crust. Here, we identify and geodynamically interpret eclogite facies metamorphism in the Triassic–Jurassic volcano-sedimentary series of the West Circum Rhodope zone in the eastern Hellenides. Equilibrium phase diagrams and measured mineral compositions were used to inform reconstructions of geodynamic evolution during the early Alpine period. We newly define the existence of the Eohellenic HP belt, consisting of pre-Alpine basement, continental volcano-sedimentary formations, and a Jurassic magmatic arc. We suggest that the Eohellenic HP-Belt was subducted in the late Jurassic to early Cretaceous beneath the European plate margin. Detailed geodynamic reconstructions such as ours provide a robust anchor for future computational models of long-term crustal evolution in the Eastern Hellenides.
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| doi_str_mv | 10.1007/s00531-023-02368-5 |
| format | Article |
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Here, we identify and geodynamically interpret eclogite facies metamorphism in the Triassic–Jurassic volcano-sedimentary series of the West Circum Rhodope zone in the eastern Hellenides. Equilibrium phase diagrams and measured mineral compositions were used to inform reconstructions of geodynamic evolution during the early Alpine period. We newly define the existence of the Eohellenic HP belt, consisting of pre-Alpine basement, continental volcano-sedimentary formations, and a Jurassic magmatic arc. We suggest that the Eohellenic HP-Belt was subducted in the late Jurassic to early Cretaceous beneath the European plate margin. Detailed geodynamic reconstructions such as ours provide a robust anchor for future computational models of long-term crustal evolution in the Eastern Hellenides.
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| subjects | Belts Continental crust Cretaceous Earth and Environmental Science Earth Sciences Eclogite Evolution Geochemistry Geology Geophysics/Geodesy Jurassic Mathematical models Metamorphism Mineral composition Mineral Resources Original Paper Phase diagrams Plate margins Sedimentary facies Sedimentology Structural Geology Triassic Volcanoes |
| title | Jurassic to early Cretaceous geodynamic evolution of the eastern Hellenides |
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