Active Magmatic Underplating in Western Eger Rift, Central Europe

The Eger Rift is an active element of the European Cenozoic Rift System associated with intense Cenozoic intraplate alkaline volcanism and system of sedimentary basins. The intracontinental Cheb Basin at its western part displays geodynamic activity with fluid emanations, persistent seismicity, Ceno...

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Veröffentlicht in:	Tectonics (Washington, D.C.) D.C.), 2017-12, Vol.36 (12), p.2846-2862
Hauptverfasser:	Hrubcová, Pavla, Geissler, Wolfram H., Bräuer, Karin, Vavryčuk, Václav, Tomek, Čestmír, Kämpf, Horst
Format:	Artikel
Sprache:	eng
Schlagworte:	active intraplate magmatic underplating Cenozoic Continental crust Crustal movement Eger Rift Fault lines Faults Fluids high‐velocity lower crust Isotope studies Isotopes Lava Magma Mantle mantle‐derived fluids Miocene Petrology Profiles Reflectance Reflection reflection‐free magma body reflectivity Refraction Sedimentary basins Seismic data Seismicity Seismological data Seismology Velocity Volcanism
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