Intraplate seismicity in the western Bohemian Massif (central Europe): A possible correlation with a paleoplate junction

• Published in: Journal of geodynamics Vol. 44; no. 3; pp. 149 - 159
• Main Authors: Babuška, V., Plomerová, J., Fischer, T.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.10.2007; Elsevier
• Subjects: Bohemian Massif; Brittle–ductile transition; Intraplate earthquake swarms; Junction of paleoplates; Junction of paleoplates; Bohemian Massif; Intraplate earthquake swarms; Brittle–ductile transition; Physical Sciences
• ISSN: 0264-3707
• DOI: 10.1016/j.jog.2007.02.004

Locations of the Eger Rift, Cheb Basin, Quaternary volcanoes, crustal earthquake swarms and exhalation centers of CO 2 and 3He of mantle origin correlate with the tectonic fabric of the mantle lithosphere modelled from seismic anisotropy. We suggest that positions of the seismic and volcanic phenomena, as well as of the Cenozoic sedimentary basins, correlate with a “triple junction” of three mantle lithospheres distinguished by different orientations of their tectonic fabric consistent within each unit. The three mantle domains most probably belong to the originally separated microcontinents – the Saxothuringian, Teplá-Barrandian and Moldanubian – assembled during the Variscan orogeny. Cenozoic extension reactivated the junction and locally thinned the crust and mantle lithosphere. The rigid part of the crust, characterized by the presence of earthquake foci, decoupled near the junction from the mantle probably during the Variscan. The boundaries (transitions) of three mantle domains provided open pathways for Quaternary volcanism and the ascent of 3He- and CO 2-rich fluids released from the asthenosphere. The deepest earthquakes, interpreted as an upper limit of the brittle–ductile transition in the crust, are shallower above the junction of the mantle blocks (at about 12 km) than above the more stable Saxothuringian mantle lithosphere (at about 20 km), probably due to a higher heat flow and presence of fluids.