About: Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation

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rdf:type	Item
description	article (en) հոդված (hy) wetenschappelijk artikel (nl) наукова стаття, опублікована у вересні 2011 (uk) article scientifique publié en 2011 (fr) im September 2011 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q60722286-25D98D9F-7BEB-4E6D-B992-58D5E9B87131
publication date	2011-09-04 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q60722286-336C4BE3-DCD2-4B29-AB9E-F34B48986399
language of work or name	English
exact match	wds:Q60722286-F140DF93-3EB7-4F1E-B3AB-DADFDC236B7A
exact match	https://scigraph.springernature.com/pub.10.1038/ngeo1250
cites work	wds:Q60722286-15243CE5-8116-4215-92AC-2FD6D943B38B wds:Q60722286-186B0142-4DE1-4F27-B120-F40CE867FE6A wds:Q60722286-1B21BD16-631D-478D-BBE5-D090FE7494CE wds:Q60722286-200995CD-39C2-428B-94A6-820852583AE2 wds:Q60722286-262AA474-B76D-4DA5-BE55-4EB138C298BC wds:Q60722286-36EF2430-C5EA-4654-8A37-7918599E59F8 wds:Q60722286-4889FC32-DB8B-48D7-BAA0-85B8548872D0 wds:Q60722286-9651B9B1-4FB3-45A7-916A-B1D99D6DE475 wds:Q60722286-A43256C7-A415-4F94-BAE9-364E27A13F99 wds:Q60722286-B0ABDF9D-6553-4B5E-A718-16CFA87857B6 wds:Q60722286-D0964392-75EB-4E31-A93E-4A7EB6436D66 wds:Q60722286-DF120662-81EC-46B2-9024-184975564C1B wds:Q60722286-E7861CBA-DA8A-4DEA-82CF-6CD4BF9239A4 wds:Q60722286-FCA707B7-7BEE-4224-89ED-03DBB7100456
cites work	Sea-floor spreading and continental drift Chemical Geodynamics Whole-mantle convection and the transition-zone water filter Recycling lower continental crust in the North China craton. Approximation of terrestrial lead isotope evolution by a two-stage model Subducting slabs stagnant in the mantle transition zone Hydrous modified spinel, Mg1.75SiH0.5O4: A new water reservoir in the mantle transition region Water transport into the deep mantle and formation of a hydrous transition zone Seismic image and origin of the Changbai intraplate volcano in East Asia: Role of big mantle wedge above the stagnant Pacific slab The role of water in the deep upper mantle and transition zone: dehydration of stagnant slabs and its effects on the big mantle wedge Water distribution across the mantle transition zone and its implications for global material circulation Stagnant slab, wet plumes and Cenozoic volcanism in East Asia Lamproites from Gaussberg, Antarctica: Possible Transition Zone Melts of Archaean Subducted Sediments Influence of temperature, composition, silica activity and oxygen fugacity on the H2O storage capacity of olivine at 8 GPa
author name string	wds:Q60722286-05E85CAE-4391-45ED-BAAA-36A369174EF0
author name string	Takeshi Kuritani
rdfs:label	Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (en) Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (nl)
skos:prefLabel	Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (en) Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (nl)
name	Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (en) Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (nl)
author	wds:Q60722286-3247F69D-060D-40A3-9386-3B6813723440 wds:Q60722286-BA6888D2-A5A1-403D-A58D-1E04768999F6
author	Eiji Ōtani Jun-Ichi Kimura
title	wds:Q60722286-B284D685-E4CA-4FF0-A641-EEF97CA37DC4
title	Intensive hydration of the mantle transition zone beneath China caused by ancient slab stagnation (en)
page(s)	wds:Q60722286-93E2AD87-7A5E-4654-88AB-54698D7AB7A2
page(s)	713-716
instance of	wds:Q60722286-A8F423D5-7533-4850-B48D-82A8CF6E2127
instance of	scholarly article
published in	wds:Q60722286-D8613131-9341-4108-9E30-72C0D61E0382
published in	Nature Geoscience
issue	wds:Q60722286-2BCD72A7-97C3-4703-8966-80C798E587C0
volume	wds:Q60722286-589FF491-ECFA-4FF4-966A-C1A1AEF2F83D
issue	10
volume	4
DOI	wds:Q60722286-1367490D-58A6-4713-9D1E-B1DF69AFAE81
DOI	http://dx.doi.org/10.1038/NGEO1250
DOI	10.1038/NGEO1250
ADS bibcode	wds:Q60722286-F0B23CC7-128B-4746-B5F4-49F90DF14300
ADS bibcode	2011NatGe...4..713K
Dimensions Publication ID	wds:Q60722286-A207A7BF-0CF1-4560-B2C1-E1395795F3A5
Dimensions Publication ID	1052963864
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q60722286
is cites work of	P and S wave tomography and anisotropy in Northwest Pacific and East Asia: Constraints on stagnant slab and intraplate volcanism Continental flood basalts derived from the hydrous mantle transition zone. Seismic Structure of the Upper Mantle Beneath Eastern Asia From Full Waveform Seismic Tomography Seismic Evidence for a Mantle Transition Zone Origin of the Wudalianchi and Halaha Volcanoes in Northeast China Mantle Transition Zone Structure Beneath Northeast Asia From 2‐D Triplicated Waveform Modeling: Implication for a Segmented Stagnant Slab Intraplate volcanism originating from upwelling hydrous mantle transition zone The role of harzburgite layers in the morphology of subducting plates and the behavior of oceanic crustal layers Buoyant hydrous mantle plume from the mantle transition zone Lithospheric Alteration, Intraplate Crustal Deformation, and Topography in Eastern China Decarbonation of Stagnant Slab in the Mantle Transition Zone Major, trace element, and Sr–Nd isotopic geochemistry of Cenozoic basalts in Central‐North and East Mongolia: Petrogenesis and tectonic implication
is cites work of	wds:Q60709082-7E92DB80-7E0D-49BE-8511-153E372EEAC1 wds:Q62701901-5F478AFE-8DD3-4C13-B4A1-531CDD82AC64 wds:Q107268896-EFD80158-DC87-4110-902C-06296DAAB29E wds:Q64091129-4D48D696-A45C-475D-874A-953B5461D4E1 wds:Q89901028-9354B68F-88AD-48CF-8C58-3143526B8B12 wds:Q43528363-A10994A9-144E-4913-877E-8417E5AF1F06 wds:Q59841977-C0D4CBEF-2D23-4F42-9A55-B7399260CA63 wds:Q107268903-E0A5F0A2-164B-4F6E-841D-B2BB086D8603 wds:Q107269151-2B786B1B-5B81-4EEC-96A3-203BCC1F0457 wds:Q66742532-F01EAAF2-930C-4AC1-BC8A-4B2E1B454E36 wds:Q59830642-F121B6E2-12D3-45B1-B6E4-8D25D6575E52

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