About: Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials

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About: Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials Goto Sponge NotDistinct Permalink

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rdf:type	Item
description	wetenschappelijk artikel (nl) article scientifique publié en 2010 (fr) наукова стаття, опублікована в лютому 2010 (uk) im Februar 2010 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q60719977-573A64E4-280F-40D3-88D7-39BB10714EFB
publication date	2010-02-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q60719977-3FFAA328-8FC6-4BF6-A735-A1069654B08E
language of work or name	English
author name string	wds:Q60719977-2F9C4FDD-B537-4E52-A985-652033D8F1E8 wds:Q60719977-336DA663-E6B3-49C3-9A77-3C0073A81943 wds:Q60719977-C12BF35B-F8BB-4DC8-A2E0-6FA1F1365561 wds:Q60719977-C1C58993-5051-483F-88EC-16C269E8888B
author name string	Tomomi Okada Junichi Nakajima Toru Matsuzawa Saeko Kita
rdfs:label	Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (en) Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (nl)
skos:prefLabel	Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (en) Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (nl)
name	Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (en) Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (nl)
author	wds:Q60719977-91079E99-7483-4BF9-8D0A-8542CEB4F5C7
author	Akira Hasegawa
title	wds:Q60719977-9FDAA617-E432-429F-A558-6BC1097D93D7
title	Anomalous deepening of a seismic belt in the upper-plane of the double seismic zone in the Pacific slab beneath the Hokkaido corner: Possible evidence for thermal shielding caused by subducted forearc crust materials (en)
page(s)	wds:Q60719977-101826B0-80A0-46E7-8574-46C55C40FAB3
page(s)	415-426
instance of	wds:Q60719977-F993BC71-0C35-4A92-BA60-6545E55D28BE
instance of	scholarly article
published in	wds:Q60719977-80B3BD51-A597-4693-8619-50CAF5D2256E
published in	Earth and Planetary Science Letters
issue	wds:Q60719977-240CF880-8929-4975-889D-EB6F944FD9DB
volume	wds:Q60719977-A2F32751-23A0-41AE-BA8B-D44DBB82B2F4
issue	3-4
volume	290
DOI	wds:Q60719977-2DC2BF57-0EC4-4C00-8B58-12E43E018C38
DOI	http://dx.doi.org/10.1016/J.EPSL.2009.12.038
DOI	10.1016/J.EPSL.2009.12.038
ADS bibcode	wds:Q60719977-2827AD2A-8308-4AC4-A6A5-6558AD07792E
ADS bibcode	2010E&PSL.290..415K
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q60719977
is cites work of	Large fault slip peaking at trench in the 2011 Tohoku-oki earthquake. Mechanism of subsidence of the Northeast Japan forearc during the late period of a gigantic earthquake cycle Prevalence of viscoelastic relaxation after the 2011 Tohoku-oki earthquake. Unusual shallow normal-faulting earthquake sequence in compressional northeast Japan activated after the 2011 off the Pacific coast of Tohoku earthquake Earthquake Impact on Active Margins: Tracing Surficial Remobilization and Seismic Strengthening in a Slope Sedimentary Sequence Compliant Volcanic Arc and Backarc Crust in Southern Kurile Suggested by Interseismic Geodetic Deformation High-resolution seismic velocity structure beneath the Hokkaido corner, northern Japan: Arc-arc collision and origins of the 1970 M 6.7 Hidaka and 1982 M 7.1 Urakawa-oki earthquakes Physical mechanisms of oceanic mantle earthquakes: Comparison of natural and experimental events Radial and Azimuthal Anisotropy Tomography of the NE Japan Subduction Zone: Implications for the Pacific Slab and Mantle Wedge Dynamics A new concept for the genesis of felsic magma: the separation of slab-derived supercritical liquid Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers
is cites work of	wds:Q64074278-BF4B2463-BDA5-4860-AE99-3E5C64E0A236 wds:Q96679100-6CFED447-B98D-419D-A5A6-E984732FEFBA wds:Q60719961-9B589CAB-37A5-4C01-A518-2D268110C6C1 wds:Q41959586-B12D140F-E5BE-4F78-99D8-C4F6951C4DB5 wds:Q59329379-96301492-4913-4FCF-8BE3-03B229615E70 wds:Q73303663-E8178CEA-A135-4BE7-AFFA-E617B74000EF wds:Q30364318-0D95C563-597B-46F0-B797-53F86AE50C04 wds:Q60704381-E0605B12-2A65-4082-9441-09F0247D286D wds:Q60699195-75C75F8A-F485-49C7-9D46-574E671929F6 wds:Q95840026-2AB7327A-4610-419E-9698-BC641E737F51 wds:Q101564218-D845F870-AA20-4723-9BB3-163EC859B2E9

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