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pro vyhledávání: '"Anna Platz"'
The Radio-Magnetotelluric (RMT) method is a geophysical near-surface imaging technique with a broad range of possible applications. In 2020, the GFZ Potsdam has acquired a newly developed horizontal magnetic dipole transmitter that allows the applica
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a870d48b7bb70e043c21ce5cd40d9cb
https://doi.org/10.5194/egusphere-egu23-917
https://doi.org/10.5194/egusphere-egu23-917
The Bohemian Massif is part of the geodynamically active European Cenozoic Rift System and represents its easternmost termination. The study area is situated at the junction of three different Variscan tectonic units and hosts beside the Eger Rift a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a99111c555e9e59c81f9de2a48c05682
https://doi.org/10.5194/egusphere-egu22-4884
https://doi.org/10.5194/egusphere-egu22-4884
Autor:
Anna Platz, Ute Weckmann, Josef Pek, Světlana Kováčiková, Radek Klanica, Johannes Mair, Basel Aleid
Publikováno v:
Tectonophysics
The region of West Bohemia and Upper Palatinate belongs to the West Bohemian Massif. The study area is situated at the junction of three different Variscan tectonic units and hosts the ENE-WSW trending Ohře Rift as well as many different fault syste
Autor:
Johannes Mair, Ute Weckmann, Radek Klanica, Basel Aleid, Anna Platz, Paula Rulff, Svetlana Kováčiková, Gregor Willkommen
The Bohemian Massif represents the easternmost part of the geodynamically active European Cenozoic Rift System. This region hosts the contact between three tectonic units of the Variscan Belt, the NE-SW trending Eger Rift and the NNW-SSE striking Mar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9e9fff355e82158d1d68c30554bbeea8
https://doi.org/10.5194/egusphere-egu21-12081
https://doi.org/10.5194/egusphere-egu21-12081
As part of the Bohemian Massif, the Cheb Basin is one of the most active areas of the European Cenozoic Rift System. Separated from the ENE-WSW striking Eger Rift to the west by the morphological prominent Mariánské Lázne Fault Zone (MLF), the bas
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df6a3d32855e0d8b129c13fff7bb61fe
https://doi.org/10.5194/egusphere-egu2020-460
https://doi.org/10.5194/egusphere-egu2020-460