Deep structure of the Bohemian Massif revealed by geophysical methods
Among the geophysical methods studying deep structure of the crust and mantle lithosphere of the Bohemian Massif (BM) are airborne magnetic and gamma-ray spectrometric as well as ground gravity survey, seismic refraction profiling, teleseismic tomography and investigation of seismic anisotropy. The gravity surveys contributed to a better knowledge of several granitic plutons, the characteristic phenomena of the BM. The seismological studies focused mainly on the deep structure of the Ohře (Eger) Graben, a prominent tectonic feature known by its abundant Cenozoic volcanism and a present-day geodynamic activity in its western part.
Journal of Geosciences, volume 63 (2018), issue 3, pages 227 - 251
Detail | full text (PDF, 2.52 MB) | references | Supplementary material
Journal of Geosciences, volume 63 (2018), issue 1, pages 3 - 20
Detail | full text (PDF, 1.79 MB) | references | Supplementary material
Journal of Geosciences, volume 57 (2012), issue 2, pages 65 - 85
Journal of Geosciences, volume 56 (2011), issue 2, pages 143 - 162
Mantle lithosphere control of crustal tectonics and magmatism of the western Ohře (Eger) Rift
Journal of Geosciences, volume 55 (2010), issue 3, pages 171 - 186
Journal of Geosciences, volume 55 (2010), issue 3, pages 187 - 199
Journal of Geosciences, volume 55 (2010), issue 3, pages 217 - 229
Gravity response of igneous rocks in the northwestern part of the Bohemian Massif
Journal of Geosciences, volume 54 (2009), issue 4, pages 325 - 342
Journal of Geosciences, volume 52 (2007), issue 3-4, pages 181 - 197