Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Joshua D. Vaughan-Hammon"'
Publikováno v:
Swiss Journal of Geosciences, Vol 114, Iss 1, Pp 1-26 (2021)
Abstract The Monte Rosa nappe consists of a wide range of lithologies that record conditions associated with peak Alpine metamorphism. While peak temperature conditions inferred from previous studies largely agree, variable peak pressures have been e
Externí odkaz:
https://doaj.org/article/9baff68c7c4445a8879a9505295d4ff3
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 23, Iss 8, Pp n/a-n/a (2022)
Abstract The distribution of metamorphic rocks throughout the western European Alps indicates subduction‐related metamorphism. However, processes by which high‐grade metamorphic rocks exhume remain disputed. Here, we present two‐dimensional pet
Externí odkaz:
https://doaj.org/article/a66297692f434920ab2f5351c85faeba
Publikováno v:
Journal of Metamorphic Geology
Journal of Metamorphic Geology, 2021, 39 (7), pp.897-917. ⟨10.1111/jmg.12595⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2021, 39 (7), pp.897-917. ⟨10.1111/jmg.12595⟩
Journal of Metamorphic Geology, 2021, 39 (7), pp.897-917. ⟨10.1111/jmg.12595⟩
Journal of Metamorphic Geology, Wiley-Blackwell, 2021, 39 (7), pp.897-917. ⟨10.1111/jmg.12595⟩
International audience; The tectono-metamorphic evolution of the European Alps is still contentious. The Monte Rosa tectonic unit is a prominent nappe in the Central European Alps and estimates of its peak Alpine pressure (P) and temperature (T) cond
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::01787c171bfe0ce545532b6cc5103df4
https://doi.org/10.1111/jmg.12595
https://doi.org/10.1111/jmg.12595
Publikováno v:
Journal of Metamorphic Geology. 39
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d0acbb889dc643657862e3840f599d46
https://doi.org/10.1111/jmg.12631
https://doi.org/10.1111/jmg.12631
Publikováno v:
European Geosciences Union General Assembly 2021 (EGU 2021)
European Geosciences Union General Assembly 2021 (EGU 2021), Apr 2021, online, Austria. ⟨10.5194/egusphere-egu21-11119⟩
European Geosciences Union General Assembly 2021 (EGU 2021), Apr 2021, online, Austria., ⟨10.5194/egusphere-egu21-11119⟩
European Geosciences Union General Assembly 2021 (EGU 2021), Apr 2021, online, Austria. ⟨10.5194/egusphere-egu21-11119⟩
European Geosciences Union General Assembly 2021 (EGU 2021), Apr 2021, online, Austria., ⟨10.5194/egusphere-egu21-11119⟩
Ultrahigh-pressure (UHP) continental crustal rocks were first discovered in the Western Alps in 1984 and have since then been observed at many convergent plate boundaries worldwide. Unveiling the processes leading to the formation and exhumation of (
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::589cc8dd962b9644313291853d4d0f60
https://hal-insu.archives-ouvertes.fr/insu-03226356
https://hal-insu.archives-ouvertes.fr/insu-03226356
Subduction zones are one of the main features of plate tectonics, they are essential for geochemical cycling and are often a key player during mountain building. However, several processes related to subduction zones remain elusive, such as the initi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad9bbd8e8ee9b3d754e59d386dda95d3
https://doi.org/10.5194/egusphere-egu21-10097
https://doi.org/10.5194/egusphere-egu21-10097
Pressure recorded in metamorphic rocks is typically assumed to represent a hydrostatic stress and thus depends linearly on depth. Recently, work in the Monte Rosa nappe in the western Alps has challenged this lithostatic assumption. Observable pressu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4ae825db0e597aba61d9db70d1739798
https://doi.org/10.5194/egusphere-egu2020-8284
https://doi.org/10.5194/egusphere-egu2020-8284