A great earthquake rupture across a rapidly evolving three-plate boundary.
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Variable Holocene deformation above a shallow subduction zone extremely close to the trenchSystematic deficiency of aftershocks in areas of high coseismic slip for large subduction zone earthquakes.Source Models and Near-Field Impact of the 1 April 2007 Solomon Islands TsunamiContinental breakup and UHP rock exhumation in action: GPS results from the Woodlark Rift, Papua New Guinea
P2860
A great earthquake rupture across a rapidly evolving three-plate boundary.
description
2009 nî lūn-bûn
@nan
2009 թուականի Ապրիլին հրատարակուած գիտական յօդուած
@hyw
2009 թվականի ապրիլին հրատարակված գիտական հոդված
@hy
2009年の論文
@ja
2009年論文
@yue
2009年論文
@zh-hant
2009年論文
@zh-hk
2009年論文
@zh-mo
2009年論文
@zh-tw
2009年论文
@wuu
name
A great earthquake rupture across a rapidly evolving three-plate boundary.
@ast
A great earthquake rupture across a rapidly evolving three-plate boundary.
@en
A great earthquake rupture across a rapidly evolving three-plate boundary.
@nl
type
label
A great earthquake rupture across a rapidly evolving three-plate boundary.
@ast
A great earthquake rupture across a rapidly evolving three-plate boundary.
@en
A great earthquake rupture across a rapidly evolving three-plate boundary.
@nl
prefLabel
A great earthquake rupture across a rapidly evolving three-plate boundary.
@ast
A great earthquake rupture across a rapidly evolving three-plate boundary.
@en
A great earthquake rupture across a rapidly evolving three-plate boundary.
@nl
P356
P1433
P1476
A great earthquake rupture across a rapidly evolving three-plate boundary.
@en
P2093
Charles J Ammon
Thorne Lay
P304
P356
10.1126/SCIENCE.1167476
P407
P577
2009-04-01T00:00:00Z