Where does subduction initiate and cease? A global scale perspective
dc.contributor.author
Ulvrova, Martina M.
dc.contributor.author
Coltice, Nicolas
dc.contributor.author
Williams, Simon
dc.contributor.author
Tackley, Paul J.
dc.date.accessioned
2019-10-08T08:58:03Z
dc.date.available
2019-10-08T02:44:00Z
dc.date.available
2019-10-08T08:58:03Z
dc.date.issued
2019-12-15
dc.identifier.issn
0012-821X
dc.identifier.issn
1385-013X
dc.identifier.other
10.1016/j.epsl.2019.115836
en_US
dc.identifier.uri
http://hdl.handle.net/20.500.11850/368956
dc.language.iso
en
en_US
dc.publisher
Elsevier
en_US
dc.subject
subduction initiation
en_US
dc.subject
subduction zones
en_US
dc.subject
mantle convection
en_US
dc.subject
plate tectonics
en_US
dc.subject
tectonic reconstructions
en_US
dc.subject
numerical simulations
en_US
dc.title
Where does subduction initiate and cease? A global scale perspective
en_US
dc.type
Journal Article
dc.date.published
2019-10-02
ethz.journal.title
Earth and Planetary Science Letters
ethz.journal.volume
528
en_US
ethz.journal.abbreviated
Earth Planet. Sci. Lett.
ethz.pages.start
115836
en_US
ethz.size
12 p.
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
2019-10-08T02:44:04Z
ethz.source
SCOPUS
ethz.eth
yes
en_US
ethz.availability
Metadata only
en_US
ethz.rosetta.installDate
2019-10-08T08:58:13Z
ethz.rosetta.lastUpdated
2022-03-28T23:49:38Z
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true
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true
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