Understanding the isotopic and chemical evolution of Yellowstone hot spot magmatism using magmatic-thermomechanical modeling
dc.contributor.author
Colón, Dylan P.
dc.contributor.author
Bindeman, Ilya N.
dc.contributor.author
Gerya, Taras
dc.date.accessioned
2019-01-18T09:48:35Z
dc.date.available
2019-01-03T03:58:47Z
dc.date.available
2019-01-18T09:48:35Z
dc.date.issued
2019-01-15
dc.identifier.issn
0377-0273
dc.identifier.issn
1872-6097
dc.identifier.other
10.1016/j.jvolgeores.2018.12.003
en_US
dc.identifier.uri
http://hdl.handle.net/20.500.11850/313489
dc.language.iso
en
en_US
dc.publisher
Elsevier
en_US
dc.subject
Thermomechanical modeling
en_US
dc.subject
Oxygen isotopes
en_US
dc.subject
Hafnium isotopes
en_US
dc.subject
Hot-spot magmatism
en_US
dc.title
Understanding the isotopic and chemical evolution of Yellowstone hot spot magmatism using magmatic-thermomechanical modeling
en_US
dc.type
Journal Article
dc.date.published
2018-01-13
ethz.journal.title
Journal of Volcanology and Geothermal Research
ethz.journal.volume
370
en_US
ethz.journal.abbreviated
J. volcanol. geotherm. res.
ethz.pages.start
13
en_US
ethz.pages.end
30
en_US
ethz.identifier.wos
ethz.identifier.scopus
ethz.publication.place
Amsterdam
en_US
ethz.publication.status
published
en_US
ethz.leitzahl
ETH Zürich::00002 - ETH Zürich::00012 - Lehre und Forschung::00007 - Departemente::02330 - Dep. Erd- und Planetenwissenschaften / Dep. of Earth and Planetary Sciences::02506 - Institut für Geophysik / Institute of Geophysics::03698 - Tackley, Paul / Tackley, Paul
ethz.leitzahl.certified
ETH Zürich::00002 - ETH Zürich::00012 - Lehre und Forschung::00007 - Departemente::02330 - Dep. Erd- und Planetenwissenschaften / Dep. of Earth and Planetary Sciences::02506 - Institut für Geophysik / Institute of Geophysics::03698 - Tackley, Paul / Tackley, Paul
ethz.date.deposited
2019-01-03T03:58:50Z
ethz.source
SCOPUS
ethz.eth
yes
en_US
ethz.availability
Metadata only
en_US
ethz.rosetta.installDate
2019-01-18T09:48:43Z
ethz.rosetta.lastUpdated
2022-03-28T22:05:43Z
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true
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true
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