Zobrazeno 1 - 8
of 8
pro vyhledávání: '"David Floess"'
Publikováno v:
Journal of petrology (2021)
The Takidani pluton (1·1–1·6 Ma) represents a shallow magmatic reservoir at the base of an exhumed caldera floor. The deposits of two large caldera-forming eruptions, the Nyukawa Pyroclastic Flow Deposit (1·76 Ma; crystal-rich dacite) and the Ch
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db304a26f86f5c3cc07e15a53f362ff0
https://archive-ouverte.unige.ch/unige:155343
https://archive-ouverte.unige.ch/unige:155343
Autor:
Kalin Kouzmanov, David Floess, Simon Wallis, Satoru Harayama, Massimo Chiaradia, Eva Hartung, Luca Caricchi
Publikováno v:
Journal of Petrology
Journal of Petrology, Vol. 58, No 4 (2017) pp. 763-788
Journal of Petrology, Vol. 58, No 4 (2017) pp. 763-788
The Takidani pluton represents one of a few locations where melt extraction from a crystal mush is preserved in the natural rock record, making it an extremely good case study for investigating the generation of evolved melt reservoirs in the upper c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0f54934c44aa8d242c757b2d8cd36732
https://doi.org/10.1093/petrology/egx033
https://doi.org/10.1093/petrology/egx033
Publikováno v:
Contributions to Mineralogy and Petrology, Vol. 174, No 27 (2019)
The separation of melt from crystals is a fundamental process driving the chemical differentiation of magmas and can lead to the formation of pockets of potentially eruptible magmas in highly crystallised magma reservoirs. While geochemical and geoph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ee2d61e650a791d7ee0c3aa44fc581b7
https://doi.org/10.1007/s00410-019-1563-9
https://doi.org/10.1007/s00410-019-1563-9
Autor:
Lukas P. Baumgartner, David Floess
Publikováno v:
Geological Society, London, Special Publications. 422:41-56
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c45e27bda755b90b585fe3812d2ab3dd
https://doi.org/10.1144/sp422.8
https://doi.org/10.1144/sp422.8
Publikováno v:
Earth and Planetary Science Letters, vol. 409, pp. 147-156
Earth and Planetary Science Letters, Vol. 409 (2015) pp. 147-156
Earth and Planetary Science Letters, Vol. 409 (2015) pp. 147-156
Melting experiments available in the literature show that carbonates and pelites melt at similar conditions in the crust. While partial melting of pelitic rocks is common and well-documented, reports of partial melting in carbonates are rare and ambi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::96e4f0386d7f5887980404121083d9c5
https://doi.org/10.1016/j.epsl.2014.10.031
https://doi.org/10.1016/j.epsl.2014.10.031
Autor:
David Floess, Lukas P. Baumgartner
Publikováno v:
Terra Nova. 25:144-150
Pre-Alpine garnets of Variscan age from metapelitic basement units in Northern Italy were strongly retrogressed at near-surface conditions prior to Alpine contact metamorphism. The replacement by sheet silicates caused a significant volume increase d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::34eecfc0abf662f627a0e013f349dbd0
https://doi.org/10.1111/ter.12018
https://doi.org/10.1111/ter.12018
Publikováno v:
Tectonophysics
Tectonophysics, Vol. 642 (2015) pp. 1-15
Tectonophysics, Vol. 642 (2015) pp. 1-15
The link between the macroscopic silicate fabric and the magnetite-controlled AMS (anisotropy of magnetic susceptibility) fabric in ferromagnetic rocks was investigated through a comprehensive comparison between different fabric measurement technique
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c6c969bd0237970a08432e1aef681f72
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:856896
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:856896
Publikováno v:
Journal of Geophysical Research. B: Solid Earth and Planets, Vol. 119, No 9 (2014) pp. 6936-6957
A major factor determining the explosivity of silicic eruptions is the removal of volatiles from magma through permeability-controlled outgassing. We studied the microstructural development of permeability during deformation of highly viscous magma b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bafe41e0991d251bcfa2c0dc84fd13b0
https://archive-ouverte.unige.ch/unige:76987
https://archive-ouverte.unige.ch/unige:76987