Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity
about
Upper- and mid-mantle interaction between the Samoan plume and the Tonga-Kermadec slabs.Mantle dynamics inferred from the crystallographic preferred orientation of bridgmanite.Evidence for a Fe3+-rich pyrolitic lower mantle from (Al,Fe)-bearing bridgmanite elasticity data.Melting temperatures of MgO under high pressure by micro-texture analysisHorizontal mantle flow controls subduction dynamics.A recent deep earthquake doublet in light of long-term evolution of Nazca subduction.On the consistency of seismically imaged lower mantle slabsBroad plumes rooted at the base of the Earth's mantle beneath major hotspots.Intraoceanic subduction spanned the Pacific in the Late Cretaceous-Paleocene.Imaging paleoslabs in the D″ layer beneath Central America and the Caribbean using seismic waveform inversion.Stability of ferrous-iron-rich bridgmanite under reducing midmantle conditions.Seismic evidence for partial melting at the root of major hot spot plumes.Sound velocities of aluminum-bearing stishovite in the mantle transition zone
P2860
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P2860
Subducted slabs stagnant above, penetrating through, and trapped below the 660 km discontinuity
description
2013 թուականի Նոյեմբերին հրատարակուած գիտական յօդուած
@hyw
2013 թվականի նոյեմբերին հրատարակված գիտական հոդված
@hy
artículu científicu espublizáu en 2013
@ast
scientific article (publication date: November 2013)
@en
wetenschappelijk artikel (gepubliceerd in 2013-11)
@nl
наукова стаття, опублікована в листопаді 2013
@uk
مقالة علمية (نشرت في نوفمبر 2013)
@ar
name
Subducted slabs stagnant above ...... below the 660 km discontinuity
@ast
Subducted slabs stagnant above ...... below the 660 km discontinuity
@en
type
label
Subducted slabs stagnant above ...... below the 660 km discontinuity
@ast
Subducted slabs stagnant above ...... below the 660 km discontinuity
@en
prefLabel
Subducted slabs stagnant above ...... below the 660 km discontinuity
@ast
Subducted slabs stagnant above ...... below the 660 km discontinuity
@en
P2860
P356
P1476
Subducted slabs stagnant above ...... below the 660 km discontinuity
@en
P2093
Masayuki Obayashi
Yoshio Fukao
P2860
P304
P356
10.1002/2013JB010466
P577
2013-11-01T00:00:00Z