Zobrazeno 1 - 10
of 118
pro vyhledávání: '"Dielforder A"'
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
Publikováno v:
In Tectonophysics 24 January 2024 871
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:
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
Autor:
Gian Maria Bocchini, Armin Dielforder, Kilian B. Kemna, Rebecca M. Harrington, Andrea Hampel, Onno Oncken
Stress in active subduction forearcs is controlled primarily by friction along the megathrust and the gravitational force. The competing deviatoric compressive and tensional stresses generated by megathrust friction and gravity, respectively, are of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66b425739b71176b8ca771ba878ea780
https://doi.org/10.5194/egusphere-egu23-3401
https://doi.org/10.5194/egusphere-egu23-3401
Autor:
Rebecca M. Harrington, Yajing Liu, Hongyu Yu, Alessandro Verdecchia, Kilian B. Kemna, Gian Maria Bocchini, Armin Dielforder, Marco P. Roth, James Kirkpatrick, Elizabeth S. Cochran, Hilary Chang, Rachel E. Abercrombie
Earthquake stress drop values estimated from ground-motion spectra commonly vary by several orders of magnitude, particularly for small earthquakes (~M < 3). Stress-drop values have been found to vary with faulting style, faulting type (intraplate, i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c0b3996a5bb05d734078acef4e7b983
https://doi.org/10.5194/egusphere-egu23-7207
https://doi.org/10.5194/egusphere-egu23-7207
Autor:
Armin DIelforder, Gian Maria Bocchini, Kilian Kemna, Andrea Hampel, Rebecca Harrington, Onno Oncken
Large megathrust earthquakes like the 2011 Mw 9.0 Tohoku earthquake (Japan) are followed by numerous aftershocks in the subduction zone forearc overlying the seismogenic fault. The aftershocks in the forearc can include normal-faulting events despite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ba185485b140e27844443e9f5a05e2e
https://doi.org/10.5194/egusphere-egu23-8028
https://doi.org/10.5194/egusphere-egu23-8028
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