About: A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China

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rdf:type	Item
description	article (en) wetenschappelijk artikel (nl) наукова стаття, опублікована в червні 2010 (uk) article scientifique publié en 2010 (fr) im Juni 2010 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q59875218-61B8ECB3-8056-471E-AA32-CC18E426FB48
publication date	2010-06-15 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59875218-32546BC1-E21E-442C-85DC-A9401D477A52
language of work or name	English
cites work	wds:Q59875218-04307BF7-66DF-4901-95B2-F2DD94C423BD wds:Q59875218-07A3FDDC-8955-4A69-AE4D-F98423FE5087 wds:Q59875218-18E11D17-DEB0-417A-8157-310B92D97A1E wds:Q59875218-19A30AA8-61EE-4C41-BA98-A81FBFABFB9E wds:Q59875218-1A5B541D-355C-430F-A494-25E4BC7C8A6A wds:Q59875218-1DDA510F-14DC-4A2F-8152-3AD485183308 wds:Q59875218-2BFA1B11-1B55-4C36-A083-81AD0B1CC4BD wds:Q59875218-3B8A0915-ABB2-4BC9-9DA0-036622C9AFB8 wds:Q59875218-43BA3ADA-E53D-41F5-AA97-2B41B84E4B25 wds:Q59875218-54FFEEDC-4C9E-455D-987D-FEB1B1D002D5 wds:Q59875218-66F624BF-AEEA-4EA1-9A3F-124172385C44 wds:Q59875218-741CE3A1-1744-4938-A162-0181DD3F57FA wds:Q59875218-90921E84-1760-484E-8E60-290AFBBE8B8E wds:Q59875218-B5D0CA89-F676-41D2-8F83-EDDB9E481DE7 wds:Q59875218-BD4481D8-1F22-4DF8-8C09-8813555DF2FB wds:Q59875218-CB4D2ECA-D463-4DD7-838A-567EF14C3A9D wds:Q59875218-CDF82A60-B6FF-44EC-B2BA-3F86AF51FB2F wds:Q59875218-D51B929D-4365-46CD-8EFD-44AB51AC284A wds:Q59875218-E6372943-D48C-4CAE-9FFB-575EBD87B385 wds:Q59875218-FC165618-F198-43A7-9690-9BC858B08590
cites work	Multiple seismic discontinuities near the base of the transition zone in the Earth's mantle Global mapping of topography on the 660-km discontinuity Global mapping of topography on transition zone velocity discontinuities by stackingSSprecursors Computation of seismic profiles from mineral physics: the importance of the non-olivine components for explaining the 660 km depth discontinuity Postspinel transformations in the system Mg2SiO4-Fe2SiO4and some geophysical implications Solubility of water in the α, β and γ phases of (Mg,Fe)2SiO4 A detailed map of the 660-kilometer discontinuity beneath the izu-bonin subduction zone Experimentally determined postspinel transformation boundary in Mg2SiO4using MgO as an internal pressure standard and its geophysical implications Subducting slabs stagnant in the mantle transition zone Upper-mantle seismic discontinuities and the thermal structure of subduction zones Traveltimes for global earthquake location and phase identification Phase transitions in pyrolitic mantle around 670-km depth: Implications for upwelling of plumes from the lower mantle Post-spinel transition in Mg2SiO4 determined by high P–T in situ X-ray diffractometry Receiver functions in northeast China – implications for slab penetration into the lower mantle in northwest Pacific subduction zone Distinct velocity variations around the base of the upper mantle beneath northeast Asia SH velocity and compositional models near the 660-km discontinuity beneath South America and northeast Asia Effect of water on the spinel-postspinel transformation in Mg2SiO4 Phase relations in hydrous MORB at 18–28GPa: implications for heterogeneity of the lower mantle Precise determination of phase relations in pyrolite across the 660km seismic discontinuity by in situ X-ray diffraction and quench experiments Topography of the 660-km discontinuity beneath northeast China: Implications for a retrograde motion of the subducting Pacific slab
author name string	wds:Q59875218-CDF465F6-E9E3-4607-BE8C-E2A8BDF660CF
author name string	Fenglin Niu
rdfs:label	A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (en) A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (nl)
skos:prefLabel	A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (en) A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (nl)
name	A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (en) A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (nl)
author	wds:Q59875218-906A21EF-C885-4B8B-8248-E4D89A88EE78
author	Baoshan Wang
title	wds:Q59875218-FA4B75E8-799C-42F3-9AC0-B73A316B7144
title	A broad 660 km discontinuity beneath northeast China revealed by dense regional seismic networks in China (en)
instance of	wds:Q59875218-B6EE9638-490F-4ABB-8686-247A1C09885B
instance of	scholarly article
main subject	wds:Q59875218-CDCE5A33-9A7B-4DB3-B66F-823C49C8B279
main subject	aquatic science
published in	wds:Q59875218-5AD01B07-1831-4CDB-AD1D-E4A7F1B4DD98
published in	Journal of Geophysical Research
issue	wds:Q59875218-676015A2-609C-49AE-B1D7-AD398E830737
volume	wds:Q59875218-D5DB4518-1B11-4681-BB2A-DAB24C415278
issue	B6
volume	115
DOI	wds:Q59875218-B643F496-8BF3-4975-ACB0-EFA75E692B7E
DOI	http://dx.doi.org/10.1029/2009JB006608
DOI	10.1029/2009JB006608
ADS bibcode	wds:Q59875218-E2408E75-6451-469A-A6FD-641680C16BC1
ADS bibcode	2010JGRB..115.6308W
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q59875218
is cites work of	Lateral variations in SH velocity structure of the transition zone beneath Korea and adjacent regions Mantle Transition Zone Structure Beneath Northeast Asia From 2‐D Triplicated Waveform Modeling: Implication for a Segmented Stagnant Slab The 3D numerical modeling of subduction dynamics: Plate stagnation and segmentation, and crustal advection in the wet mantle transition zone
is cites work of	wds:Q62701901-C8C0D179-8648-4B28-A3E3-62DF8CE410AB wds:Q107269102-0A811331-19E9-4BF6-9AE4-1EDFEA8CD6BB wds:Q57889945-97EDD4A4-B2E8-40CE-BFC5-24F3154B3C58

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