Zobrazeno 1 - 10
of 250
pro vyhledávání: '"Magdalena Scheck‐Wenderoth"'
Autor:
Judith Bott, Magdalena Scheck-Wenderoth, Ajay Kumar, Mauro Cacace, Sebastian Noe, Jan Inge Faleide
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-14 (2024)
Abstract The distribution of earthquakes in stable intracontinental tectonic settings is typically far more diffuse than along plate boundaries and the causative mechanisms underlying some recognizable clustering are not understood. Here we show that
Externí odkaz:
https://doaj.org/article/e634c4fea1cb49c2a88d010fe9e4dbb9
Autor:
Hans-Jürgen Götze, Ronja Strehlau, Anke Dannowski, Denis Anikiev, Ajay Kumar, Magdalena Scheck-Wenderoth
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
The geodynamic evolution of the Liguro-Provençal Basin and its crust and upper mantle structure remain debated, especially regarding the role of rifting in continental break-up and seafloor spreading. Our study incorporates updated datasets, includi
Externí odkaz:
https://doaj.org/article/c6edf7006eb344ae8554cbb75f830e2b
Autor:
María Laura Gómez Dacal, Magdalena Scheck-Wenderoth, Jan Inge Faleide, Mohamed Mansour Abdelmalak, Judith Bott, Denis Anikiev
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-9 (2023)
Abstract Plumes are domains where hotter material rises through Earth´s mantle, heating also the moving lithospheric plates that may experience thinning or even continental breakup. In particular, the Iceland plume in the NE Atlantic (NEA) could hav
Externí odkaz:
https://doaj.org/article/695518ab7d9849389ae0f0bfc21c54de
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-13 (2023)
Abstract Continental deformation is known to be controlled by the interplay between tectonic and gravitational forces modulated by thermal relaxation-controlled lithospheric strength leading to oscillations around an equilibrium state, or to runaway
Externí odkaz:
https://doaj.org/article/4df0ed6e8ee64b688897e8b7e028ed8a
Publikováno v:
Frontiers in Water, Vol 6 (2024)
This study investigates the decades-long evolution of groundwater dynamics and thermal field in the North German Basin beneath Brandenburg (NE Germany) by coupling a distributed hydrologic model with a 3D groundwater model. We found that hydraulic gr
Externí odkaz:
https://doaj.org/article/3a8e1143927f4cd7b22351331f931a71
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Externí odkaz:
https://doaj.org/article/d52168d2d234489d969fa1454febd228
Autor:
Constanza Rodriguez Piceda, Ya-Jian Gao, Mauro Cacace, Magdalena Scheck-Wenderoth, Judith Bott, Manfred Strecker, Frederik Tilmann
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-10 (2023)
Seismicity in subducted slabs is principally controlled by compaction and dehydration reactions in regions of hydrated mantle and by enhanced flexural stresses in regions of anhydrous mantle, suggests an analysis of seismic tomography data from the N
Externí odkaz:
https://doaj.org/article/ae3136e340a94fcb89d6b2db80e465e3
Publikováno v:
Geothermal Energy, Vol 11, Iss 1, Pp 1-21 (2023)
Abstract One key aspect in the energy transition is to use the deep geothermal energy stored in sedimentary basins as well as in igneous and metamorphic basement rocks. To estimate the variability of deep geothermal potentials across different geolog
Externí odkaz:
https://doaj.org/article/c58fe31201e54f1ba7526e63bbacbaf5
Autor:
Steffen Ahlers, Luisa Röckel, Tobias Hergert, Karsten Reiter, Oliver Heidbach, Andreas Henk, Birgit Müller, Sophia Morawietz, Magdalena Scheck-Wenderoth, Denis Anikiev
Publikováno v:
Geothermal Energy, Vol 10, Iss 1, Pp 1-32 (2022)
Abstract Information about the absolute stress state in the upper crust plays a crucial role in the planning and execution of, e.g., directional drilling, stimulation and exploitation of geothermal and hydrocarbon reservoirs. Since many of these appl
Externí odkaz:
https://doaj.org/article/53979aa2c316471794a58c2560d28bce
Publikováno v:
Geophysical Research Letters, Vol 49, Iss 18, Pp n/a-n/a (2022)
Abstract The dynamics of the Alps and surrounding regions is still not completely understood, partly because of a non‐unique interpretation of its upper‐mantle architecture. In particular, it is unclear if interpreted slabs are consistent with th
Externí odkaz:
https://doaj.org/article/aabe1ede59234c599927b97b1570a173