Zobrazeno 1 - 10
of 254
pro vyhledávání: '"Dielforder, A."'
Publikováno v:
In Tectonophysics 24 January 2024 871
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 3, Pp n/a-n/a (2023)
Abstract Numerous normal‐faulting aftershocks in subduction forearcs commonly follow large megathrust earthquakes. Postseismic normal faulting has been explained by stress changes induced by the stress drop along the megathrust. However, details of
Externí odkaz:
https://doaj.org/article/24bfce6d3a2747d5b27066a259738826
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 9, Pp n/a-n/a (2022)
Abstract Double seismic zones (DSZs), parallel planes of intermediate‐depth earthquakes inside oceanic slabs, have been observed in a number of subduction zones and may be a ubiquitous feature of downgoing oceanic plates. Focal mechanism observatio
Externí odkaz:
https://doaj.org/article/912ebba3181941b0b00fd12d13dc71c9
Autor:
Laura V. Krone, Ferdinand J. Hampl, Christopher Schwerdhelm, Casey Bryce, Lars Ganzert, Axel Kitte, Kirstin Übernickel, Armin Dielforder, Santiago Aldaz, Rómulo Oses-Pedraza, Jeffrey Paulo H. Perez, Pablo Sanchez-Alfaro, Dirk Wagner, Ute Weckmann, Friedhelm von Blanckenburg
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-15 (2021)
Abstract The weathering front is the boundary beneath Earth’s surface where pristine rock is converted into weathered rock. It is the base of the “critical zone”, in which the lithosphere, biosphere, and atmosphere interact. Typically, this fro
Externí odkaz:
https://doaj.org/article/127a87e9c54f4c688f95e83536c76b35
Autor:
Vasso Saltogianni, Vasiliki Mouslopoulou, Armin Dielforder, Gian Maria Bocchini, Jonathan Bedford, Onno Oncken
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 11, Pp n/a-n/a (2021)
Abstract Slow slip events (SSEs) at subduction zones can precede large‐magnitude earthquakes and may serve as precursor indicators, but the triggering of earthquakes by slow slip remains insufficiently understood. Here, we combine geodetic, Coulomb
Externí odkaz:
https://doaj.org/article/c5ce6b37e39245c0b5ad17b4517c5ba9
Publikováno v:
Geological Magazine; Nov2022, Vol. 159 Issue 11/12, p2191-2205, 15p
Autor:
Ford Mary, Masini Emmanuel, Vergés Jaume, Pik Raphael, Ternois Sébastien, Léger Julien, Dielforder Armin, Frasca Gianluca, Grool Arjan, Vinciguerra Constance, Bernard Thomas, Angrand Paul, Crémades Antoine, Manatschal Gianreto, Chevrot Sébastien, Jolivet Laurent, Mouthereau Frédéric, Thinon Isabelle, Calassou Sylvain
Publikováno v:
BSGF - Earth Sciences Bulletin, Vol 193, p 19 (2022)
The Pyrenees is a collisional orogen built by inversion of an immature rift system during convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The full mountain belt consists of the pro-foreland southern Pyrenees and
Externí odkaz:
https://doaj.org/article/144460a6f8454234b2e59ba577dbe579
Autor:
Tom Dielforder, Christina Maria Braun, Fabian Hölzgen, Shuang Li, Mona Thiele, Marina Huber, Uli Ohmayer, Jorge Perez-Fernandez
Publikováno v:
Non-Coding RNA, Vol 8, Iss 1, p 1 (2022)
The synthesis of ribosomes involves the correct folding of the pre-ribosomal RNA within pre-ribosomal particles. The first ribosomal precursor or small subunit processome assembles stepwise on the nascent transcript of the 35S gene. At the earlier st
Externí odkaz:
https://doaj.org/article/75ba1be2daa345b19f37814f74fa6fd2
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Subduction zone forearcs deform transiently and permanently due to the frictional coupling with the converging lower plate. Transient stresses are mostly the elastic response to the seismic cycle. Permanent deformation is evidenced by forearc topogra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::914d97f6b7b74c663693a28129a88731
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021194
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5021194
Modern concepts of fault strength account for compositional and hence rheological heterogeneity of natural fault zones. An important implication of heterogeneity is strain partitioning between stronger and weaker phases and a gradual transition from
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ed612a37f859dc42442883e242adbd72
https://doi.org/10.5194/egusphere-egu23-4874
https://doi.org/10.5194/egusphere-egu23-4874