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作者:Petra Štěpančíková , Tomáš Fischer ...
来源:[J].Geomorphology(IF 2.552), 2018
摘要:Abstract(#br)The NNW-SSE trending Mariánské Lázně Fault (MLF) zone is situated in the western part of the Bohemian Massif (Czech Republic, central Europe) and controls the eastern limit of Cenozoic Cheb basin. The Cheb basin is well-known for present-day earthquake swarms, w...
作者:... Hector Perea , Petra Štěpančíková , Teresa Ramírez-Herrera
来源:[J].Geomorphology(IF 2.552), 2018
摘要:Abstract(#br)The Acambay Graben, within the central part of the Trans-Mexican Volcanic Belt, is one of the major sources of continental earthquakes in Mexico. To date, the activity and paleoseismological history of the axial faults of the graben are not well constrained. We ...
作者:... Vít Ambrož , Michal Urban , Petra Štěpančíková
来源:[J].Quaternary International(IF 1.962), 2017, Vol.451, pp.56-73
摘要:Abstract(#br)Successions of colluvia and loesses covering the faults in the eastern and central parts of the Bohemian Massif were exposed in six trenches (two trenches at each fault, up to 6 m deep) and studied in detail in terms of stratigraphy and deformation. Based on OSL...
作者:... Jiří Málek , Jiří Adamovič , Petra Štěpančíková
来源:[J].Journal of Geodynamics(IF 2.967), 2015, Vol.87, pp.26-49
摘要:Abstract(#br)An analysis of fault-slip data from the Lusatian Fault Belt, limiting the Lusatian Block of the Bohemian Massif in the SW, yielded parameters of eight successive paleostress patterns, Late Cretaceous to Plio-Pleistocene in age. These patterns were linked with sp...
作者:Petra Štěpančíková , Josef Stemberk ...
来源:[J].Geomorphology(IF 2.552), 2007, Vol.102 (1), pp.68-80
摘要:Abstract(#br)This paper presents results of morphotectonic research carried out in order to determine the neotectonic development of the drainage network in the NE spur of the Bohemian Massif (central Europe). The area studied comprises the north-eastern sector of the Rychle...
作者:Petra Štěpančíková , Jiří Dohnal ...
来源:[J].Journal of Applied Geophysics(IF 1.327), 2011, Vol.74 (1), pp.69-80
摘要:Abstract(#br)This paper presents the results of two separate geophysical investigations undertaken across the Sudetic Marginal Fault zone in the Bohemian Massif. This fault zone represents one of the most important tectonic features in central Europe. The first, preliminary,...
作者:Petra Štěpančíková , Jozef Hók ...
来源:[J].Tectonophysics(IF 2.684), 2010, Vol.485 (1), pp.269-282
摘要:Abstract(#br)The NW–SE striking Sudetic Marginal Fault (SMF) is one of the most conspicuous tectonic structures in central Europe. It controls the pronounced morphotectonic escarpment of the Sudetic Mountains for a length of 130 km. This paper presents the results of trenchi...
作者:Petra Štěpančíková , Jan Švancara ...
来源:[J].International Journal of Earth Sciences(IF 2.261), 2015, Vol.104 (4), pp.963-990
摘要:Abstract(#br)We give an interpretive review of the geological evolution of the Nysa-Morava Zone (NMZ)—a Late Cenozoic tectonically active region of the NE Bohemian Massif located at its contact with the Western Carpathians’ orogenic front. This crustal domain, delimited by g...
作者:Petra Štěpančíková , Magda Karousová ...
来源:[J].Studia Geophysica et Geodaetica(IF 0.975), 2012, Vol.56 (4), pp.1019-1036
摘要:Abstract(#br)Geodynamic activity in the area of West Bohemia is typified by the occurrence of earthquake swarms, Quaternary volcanism and high flux of mantle-derived CO 2 . The highest swarm activity occurs beneath the eastern edge of the Cheb basin, which is delineated by t...
作者:Petra Štěpančíková , Josef Stemberk
来源:[J].Acta Geologica Slovaca, 2010, Vol.2 (1), pp.11
摘要:The Sudetic Marginal Fault (SMF) separates the Fore-Sudetic block on the NE and the Sudetic block on the SW of Bohemian Massif. The fault slip data along the SMF yielded two different subhorizontal orientations of the maximum stress axes. The NE–SW oriented compression was c...

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