Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Pierre Mueller"'
Publikováno v:
Geosciences, Vol 10, Iss 1, p 26 (2020)
This paper reports the results of a field-based structural investigation of a well-exposed paleo-accretionary prism, which experienced complex deformation in a low-grade metamorphic setting. Field analyses focused on the description of structural fab
Externí odkaz:
https://doaj.org/article/414bd2700b684f28b1a4d8ae4ccd1e5c
Autor:
Stéphane Andrieu, Pierre Müller
La physique des surfaces est une science à la fois ancienne et récente. Ancienne parce que les premiers concepts ayant permis d'étudier les surfaces datent du début du XXe siècle. Récente parce que l'étude approfondie et systématique des surf
Publikováno v:
Italian Journal of Geosciences. 140:255-274
Transitional flow deposits (TFDs) and hybrid event beds (HEBs) form part of the high-density sediment gravity flow spectrum. They record flow characteristics intermediate between fully turbulent and laminar flow states. The transformation from initia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ef8fb2e8ef3b469ceaaef87cb55cd5d0
https://doi.org/10.3301/ijg.2020.32
https://doi.org/10.3301/ijg.2020.32
Autor:
Silvia Tamburelli, Pierre Mueller, Chiara Amadori, Laura Crispini, Matteo Maino, Niccolò Menegoni
In the time frame after initial deposition but prior to lithification, sediments are frequently prone to physical, chemical, or biological disturbance. The resultant structures – commonly referred to as soft sediment deformation (SSD) - can be expl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fff764317e3b91cc21c2a0ccc415acca
https://doi.org/10.5194/egusphere-egu22-9228
https://doi.org/10.5194/egusphere-egu22-9228
Publikováno v:
Sedimentary Geology 377 (2018): 147–161. doi:10.1016/j.sedgeo.2018.10.002
info:cnr-pdr/source/autori:Mueller P.[1], Langone A.[2], Patacci M.[3], Di Giulio A.[1]/titolo:Detrital signatures of impending collision: The deep-water record of the Upper Cretaceous Bordighera Sandstone and its basal complex (Ligurian Alps, Italy)/doi:10.1016%2Fj.sedgeo.2018.10.002/rivista:Sedimentary Geology/anno:2018/pagina_da:147/pagina_a:161/intervallo_pagine:147–161/volume:377
info:cnr-pdr/source/autori:Mueller P.[1], Langone A.[2], Patacci M.[3], Di Giulio A.[1]/titolo:Detrital signatures of impending collision: The deep-water record of the Upper Cretaceous Bordighera Sandstone and its basal complex (Ligurian Alps, Italy)/doi:10.1016%2Fj.sedgeo.2018.10.002/rivista:Sedimentary Geology/anno:2018/pagina_da:147/pagina_a:161/intervallo_pagine:147–161/volume:377
Despite intensive research efforts and significant advances in the understanding of subduction and obduction processes that affected several units which at the present day compose the Western Alps, the paleogeographic evolution of the Alpine Tethys r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2f0d25d8b82f7d69830cefbf40e3354b
https://doi.org/10.1016/j.sedgeo.2018.10.002
https://doi.org/10.1016/j.sedgeo.2018.10.002
Publikováno v:
Minerals
Volume 10
Issue 7
Minerals, Vol 10, Iss 632, p 632 (2020)
Minerals (Basel) 10 (2020). doi:10.3390/min10070632
info:cnr-pdr/source/autori:Di Giulio A.[1], Amadori C.[1], Mueller P.[1], Langone A.[2]/titolo:Role of the Down-Bending Plate as a Detrital Source in Convergent Systems Revealed by U-Pb Dating of Zircon Grains: Insights from the Southern Andes and Western Italian Alps/doi:10.3390%2Fmin10070632/rivista:Minerals (Basel)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:10
Volume 10
Issue 7
Minerals, Vol 10, Iss 632, p 632 (2020)
Minerals (Basel) 10 (2020). doi:10.3390/min10070632
info:cnr-pdr/source/autori:Di Giulio A.[1], Amadori C.[1], Mueller P.[1], Langone A.[2]/titolo:Role of the Down-Bending Plate as a Detrital Source in Convergent Systems Revealed by U-Pb Dating of Zircon Grains: Insights from the Southern Andes and Western Italian Alps/doi:10.3390%2Fmin10070632/rivista:Minerals (Basel)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:10
In convergent zones, several parts of the geodynamic system (e.g., continental margins, back-arc regions) can be deformed, uplifted, and eroded through time, each of them potentially delivering clastic sediments to neighboring basins. Tectonically dr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8ce68ee84b949fe2b8a6a4b4ecae423b
Constraining the source terranes of Alpine siliciclastic flysch sequences is crucial for building a clearer picture of the palaeogeography and geodynamic evolution of the Western Tethys in the framework of impending continental collision. This paper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::98254d61d7e9e3a6454fe1eb2c3e0fb6
https://eprints.whiterose.ac.uk/153894/1/Mueller_et_al_2020.pdf
https://eprints.whiterose.ac.uk/153894/1/Mueller_et_al_2020.pdf
Autor:
Pierre Mueller, Tom McCann
Publikováno v:
Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen. 274:55-71
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0509ef8301f5ba366ece7dca1d82af0
https://doi.org/10.1127/njgpa/2014/0439
https://doi.org/10.1127/njgpa/2014/0439
Bringing together experts from the various disciplines involved, this first comprehensive overview of the current level of stress engineering on the nanoscale is unique in combining the theoretical fundamentals with simulation methods, model systems