Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Esther Heckenbach"'
Understanding how normal fault networks initiate and evolve is important for quantifying plate boundary deformation, assessing seismic hazard and finding natural resources. In recent years, 3D numerical models have been developed that can simulate th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::913a1bfff57879a23c2221b9e41e6a94
https://doi.org/10.5194/egusphere-egu23-11050
https://doi.org/10.5194/egusphere-egu23-11050
The region around the Dead Sea Transform represents a unique example of the structures that form around restraining and releasing bends in a strike-slip environment. With our 3D numerical models, we aim to understand the processes that shaped the reg
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9d1b1243078720d500923f177e353b77
https://doi.org/10.5194/egusphere-egu22-5427
https://doi.org/10.5194/egusphere-egu22-5427
The lithosphere is often assumed to reside in a thermal steady-state when quantitatively describing the temperature distribution in continental interiors and sedimentary basins, but also at active plate boundaries. Here, we investigate the applicabil
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aab48ffe896400ea3c64a58ff9dc37ef
https://doi.org/10.31223/x5qk62
https://doi.org/10.31223/x5qk62
Publikováno v:
Journal of Structural Geology
Fault-propagation folding occurs when a shallow fold is created by an underlying propagating thrust fault. These structures are common features of fold and thrust belts and hold key economic relevance as groundwater or hydrocarbon reservoirs. Reconst
Autor:
Michael Rudolf, Joscha Podlesny, Esther Heckenbach, Matthias Rosenau, Anne Glerum, Ralf Kornhuber, Sascha Brune, Onno Oncken
The release of elastic energy along an active fault is accommodated by a wide range of slip modes. It ranges from long-term slow slip events (SSEs) and creep to short-term tremors and earthquakes. They vary not only in their characteristic duration b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5685b7d730fece7e183c7a5400b65b91
https://doi.org/10.5194/egusphere-egu21-4168
https://doi.org/10.5194/egusphere-egu21-4168
Autor:
Roberto Miele, Ben Norden, Sven Fuchs, Hans-Jürgen Förster, Niels Balling, Andrea Förster, Esther Heckenbach
Publikováno v:
Fuchs, S, Förster, H J, Norden, B, Balling, N, Miele, R, Heckenbach, E & Förster, A 2021, ' The Thermal Diffusivity of Sedimentary Rocks : Empirical Validation of a Physically Based α − φ Relation ', Journal of Geophysical Research: Solid Earth, vol. 126, no. 3, e2020JB020595 . https://doi.org/10.1029/2020JB020595
Journal of Geophysical Research: Solid Earth
Journal of Geophysical Research: Solid Earth
Understanding the thermal behavior of nonsteady state subsurface geosystems, when temperature changes over time, requires knowledge on the speed of heat propagation and, thus, of the rock's thermal diffusivity as essential thermo-physical parameter.
Autor:
Matthias Rosenau, Onno Oncken, Anne Glerum, Michael Rudolf, Ralf Kornhuber, Esther Heckenbach, Joscha Podlesny, Sascha Brune
The release of elastic energy along an active fault is accommodated by a wide range of slip modes. It ranges from long-term slow slip events (SSEs) and creep to short-term tremors and earthquakes. They vary not only in their characteristic duration b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19552ed386d994226ff157ae7293f520
https://doi.org/10.5194/egusphere-egu2020-9369
https://doi.org/10.5194/egusphere-egu2020-9369