Zobrazeno 1 - 10
of 64
pro vyhledávání: '"A. Vho"'
Publikováno v:
Solid Earth, Vol 11, Pp 307-328 (2020)
Oxygen isotope geochemistry is a powerful tool for investigating rocks that interacted with fluids, to assess fluid sources and quantify the conditions of fluid–rock interaction. We present an integrated modelling approach and the computer program
Externí odkaz:
https://doaj.org/article/4504ad8596c9498f9ec7f25b65cf52b5
Publikováno v:
Swiss Journal of Geosciences, Vol 113, Iss 1, Pp 1-33 (2020)
Abstract Microscale dating of distinct domains in minerals that contain relics of multiple metamorphic events is a key tool to characterize the polyphase evolution of complex metamorphic terranes. Zircon and allanite from five metasediments and five
Externí odkaz:
https://doaj.org/article/1bb2a47bd52a4dda9598cb9d5ff3a8c5
Autor:
Vho, Alice1 (AUTHOR) alice.vho@geo.unibe.ch, Rubatto, Daniela1,2 (AUTHOR), Putlitz, Benita2 (AUTHOR), Bouvier, Anne‐Sophie2 (AUTHOR)
Publikováno v:
Geostandards & Geoanalytical Research. Sep2020, Vol. 44 Issue 3, p459-471. 13p.
Autor:
Vho, Alice1 (AUTHOR) alice.vho@geo.unibe.ch, Lanari, Pierre1 (AUTHOR), Rubatto, Daniela1,2 (AUTHOR), Hermann, Jörg1 (AUTHOR)
Publikováno v:
Solid Earth. 2020, Vol. 11 Issue 2, p307-328. 22p.
Autor:
Daniela Rubatto, Thomas Bovay, Alice Vho, Maria Rosa Scicchitano, Pierre Lanari, Joerg Hermann
The capacity of garnet to preserve successive growth stages over the P–T evolution of the host rock remains unsurpassed. The distributions of major elements, trace elements and oxygen isotopes, can be mapped at high spatial resolution to decode thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0351a6671dbcf49ecb35a8b4803b9b24
https://doi.org/10.5194/egusphere-egu22-4248
https://doi.org/10.5194/egusphere-egu22-4248
Publikováno v:
Solid Earth. 11:307-328
Oxygen isotope geochemistry is a powerful tool for investigating rocks that interacted with fluids, to assess fluid sources and quantify the conditions of fluid–rock interaction. We present an integrated modelling approach and the computer program
Publikováno v:
Abstracts
The capacity of garnet to preserve successive growth stages over the P–T evolution of the host rock remains unsurpassed. The distributions of major elements, trace elements and oxygen isotopes, can be mapped at high spatial resolution to decode thi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______156::59963f48963116bb9197b4c1e6ae0447
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5010907
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5010907
Publikováno v:
Vho, Alice; Rubatto, Daniela; Lanari, Pierre; Giuntoli, Francesco; Regis, Daniele; Hermann, Jörg (2020). Crustal reworking and hydration: insights from element zoning and oxygen isotopes of garnet in high‑pressure rocks (Sesia Zone, Western Alps). Contributions to mineralogy and petrology, 175(11), pp. 109-137. Springer-Verlag 10.1007/s00410-020-01745-6
Subduction zones represent one of the most critical settings for fluid recycling as a consequence of dehydration of the subducting lithosphere. A better understanding of fluid flows within and out of the subducting slab is fundamental to unravel the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::888208252f8d166851f46ade058e1319
http://hdl.handle.net/11585/777017
http://hdl.handle.net/11585/777017
Publikováno v:
Vho, Alice; Lanari, Pierre; Rubatto, Daniela (2019). An internally-consistent database for oxygen isotope fractionation between minerals. Journal of petrology, 60(11), pp. 2101-2129. Oxford University Press 10.1093/petrology/egaa001
The knowledge of the fractionation behaviour between phases in isotopic equilibrium and its evolution with temperature is fundamental to assist the petrological interpretation of measured oxygen isotope compositions. We report a comprehensive and upd
Autor:
Daniela Rubatto, Jörg Hermann, Detlef Günther, Lanari Pierre, Bodo Hattendorf, Marcel Burger, Francesca Piccoli, Gunnar Schwarz, Thomas Bovay, Alice Vho
Garnet is one of the most robust and ubiquitous minerals that record element zoning during crustal metamorphism. In addition to major element distribution, zoning in trace elements can provide a wealth of information to document the changing conditio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e3ad619f84332968e49ef678c28c87d
https://doi.org/10.5194/egusphere-egu21-6050
https://doi.org/10.5194/egusphere-egu21-6050