Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Thomas Bovay"'
Autor:
Johanna Marin Carbonne, Andras Kiss, Anne-Sophie Bouvier, Anders Meibom, Lukas Baumgartner, Thomas Bovay, Florent Plane, Stephane Escrig, Daniela Rubatto
Publikováno v:
CHIMIA, Vol 76, Iss 1-2 (2022)
Secondary Ion Mass Spectrometry (SIMS) extracts chemical, elemental, or isotopic information about a localized area of a solid target by performing mass spectrometry on secondary ions sputtered from its surface by the impact of a beam of charged part
Externí odkaz:
https://doaj.org/article/5b5304f539464e8493d04ef2e555681b
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:
Contributions to Mineralogy and Petrology, vol. 176, no. 7
Contributions to Mineralogy and Petrology
Bovay, Thomas; Rubatto, Daniela; Lanari, Pierre (2021). Pervasive fluid-rock interaction in subducted oceanic crust revealed by oxygen isotope zoning in garnet. Contributions to mineralogy and petrology, 176(7) Springer-Verlag 10.1007/s00410-021-01806-4
Contributions to Mineralogy and Petrology
Bovay, Thomas; Rubatto, Daniela; Lanari, Pierre (2021). Pervasive fluid-rock interaction in subducted oceanic crust revealed by oxygen isotope zoning in garnet. Contributions to mineralogy and petrology, 176(7) Springer-Verlag 10.1007/s00410-021-01806-4
Dehydration reactions in the subducting slab liberate fluids causing major changes in rock density, volume and permeability. Although it is well known that the fluids can migrate and interact with the surrounding rocks, fluid pathways remain challeng
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ed1ff96f06586c6808e07f3bac3cdaa9
https://serval.unil.ch/notice/serval:BIB_28E2467EFD00
https://serval.unil.ch/notice/serval:BIB_28E2467EFD00
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
Autor:
Thomas Bovay, Daniela Rubatto, Nicolas Riel, Alice Vho, Thorsten Markmann, Hugo Dominguez, Pierre Lanari
Petrological models based on equilibrium thermodynamics have proven critical in assessing how mineral assemblages evolve with pressure (P) and temperature (T) conditions. Still, they remain limited for the investigation and simulation of fluid-rock i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c759978afe058e63632688e4d775be1
https://doi.org/10.5194/egusphere-egu21-7938
https://doi.org/10.5194/egusphere-egu21-7938
Publikováno v:
Goldschmidt2021 abstracts.
Publikováno v:
Journal of Metamorphic Geology
Bovay, Thomas; Lanari, Pierre; Rubatto, Daniela; Smit, Matthijs; Piccoli, Francesca (2021). Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland). Journal of metamorphic geology, 40(2), pp. 175-206. Wiley 10.1111/jmg.12623
Bovay, Thomas; Lanari, Pierre; Rubatto, Daniela; Smit, Matthijs; Piccoli, Francesca (2021). Pressure–temperature–time evolution of subducted crust revealed by complex garnet zoning (Theodul Glacier Unit, Switzerland). Journal of metamorphic geology, 40(2), pp. 175-206. Wiley 10.1111/jmg.12623
Collisional orogens commonly include mono-metamorphic and poly-metamorphic units, and their different evolution can be difficult to recognise and reconcile. The Theodul Glacier Unit (TGU) in the Western Alps consists of an association of metasediment
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba1f08a677af278713db7b80c7c5e768
Reconstructing the tectonic history of metamorphosed terranes is a key step towards establishing a comprehensive model for collisional orogens such as the Alps. Single chronometers tend to record one specific component of such history—be it inherit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46e22a206678dce3272cacd087e706b9
https://doi.org/10.5194/egusphere-egu2020-15877
https://doi.org/10.5194/egusphere-egu2020-15877
Compositional mapping has greatly impacted mineralogical and petrological studies over the past half-century with increasing use of the electron probe micro-analyser. Many technical and analytical developments have benefited from the synergies of phy
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4b233a00df240010ba9021309f1acfeb