About: Growth of early continental crust controlled by melting of amphibolite in subduction zones

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scientific article published in Nature

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rdf:type	Item
description	artículu científicu (ast) wetenschappelijk artikel (nl) article publié dans la revue scientifique Nature (fr) im Juni 2002 veröffentlichter wissenschaftlicher Artikel (de) scientific article published in Nature (en) Նեյչրում հրատարակված հոդված (hy) наукова стаття, опублікована в Nature в червні 2002 (uk)
publication date	wds:Q59059067-17E0F5EA-9BBA-4C83-A307-A0FFA3426E3C
publication date	2002-06-01 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59059067-929655BB-D995-4A50-A0C9-65973F5BC945
language of work or name	English
exact match	wds:Q59059067-46A621BB-355A-4EC5-BC5B-6E99B702390C
exact match	https://scigraph.springernature.com/pub.10.1038/nature00799
cites work	wds:Q59059067-12D22E28-E964-4F9E-A438-9F5F8A574AF3 wds:Q59059067-146A1D76-9E3F-433C-9341-9C4C47CD48EA wds:Q59059067-203397B6-EBC4-45A1-B1B3-EDCF5C93F438 wds:Q59059067-356C5A21-EF36-4C36-9D45-6342969EB725 wds:Q59059067-63F27CDD-0B8F-4647-8540-4ECFADB831A0 wds:Q59059067-8178A2AC-2C32-4EB0-9CC5-1947EDE1DD6F wds:Q59059067-847E2184-860C-41E3-A476-44F9B6CC98D7 wds:Q59059067-87599805-98F8-4823-BDE9-6B281736560F wds:Q59059067-9F77282E-AF10-4AFD-A09A-D81566229685 wds:Q59059067-A44973CF-FB8B-4F3E-ABAF-5DC62971B23D wds:Q59059067-A78569F1-646B-4CF7-B497-C7E947F1184D wds:Q59059067-AF4E2ED4-55A1-49C1-9331-703CDE8BC346 wds:Q59059067-B7ED9352-6422-4164-9CF3-B3789A6CED2B wds:Q59059067-D1C58724-D4E2-435D-A99A-CC1180DC61DB wds:Q59059067-F54A5D3D-ED3C-40FD-84F2-154929E7D24B
cites work	Rutile/melt partition coefficients for trace elements and an assessment of the influence of rutile on the trace element characteristics of subduction zone magmas Dehydration-melting of amphibolite at 10 kbar: the effects of temperature and time Evidence for Archean ocean crust with low high field strength element signature from diamondiferous eclogite xenoliths Rutile-Bearing Refractory Eclogites: Missing Link Between Continents and Depleted Mantle Ion Microprobe Study of Plagioclase-Basalt Partition Experiments at Natural Concentration Levels of Trace Elements Partial melting in Archean subduction zones: constraints from experimentally determined trace element partition coefficients between eclogitic minerals and tonalitic melts under upper mantle conditions Nb and Ta incorporation and fractionation in titanian pargasite and kaersutite: crystal–chemical constraints and implications for natural systems A model for Trondhjemite-Tonalite-Dacite Genesis and crustal growth via slab melting: Archean to modern comparisons An experimental study of trace element partitioning between olivine, orthopyroxene and melt in chondrules: equilibrium values and kinetic effects NbTa-rich mantle amphiboles and micas: Implications for subduction-related metasomatic trace element fractionations An experimental study of Nb and Ta partitioning between Ti-rich minerals and silicate liquids at high pressure and temperature Partial melting of amphibolite/eclogite and the origin of Archean trondhjemites and tonalites Determination of partition coefficients for trace elements in high pressure-temperature experimental run products by laser ablation microprobe-inductively coupled plasma-mass spectrometry (LAM-ICP-MS) Fluid- and melt-related enrichment in the subarc mantle: Evidence from Nb/Ta variations in island-arc basalts Incompatible element-rich fluids released by antigorite breakdown in deeply subducted mantle
author name string	wds:Q59059067-898FA0DE-7057-4682-9C79-2F0FB0E56C78
author name string	Riccardo Vannucci
rdfs:label	Growth of early continental crust controlled by melting of amphibolite in subduction zones (en) Growth of early continental crust controlled by melting of amphibolite in subduction zones (nl)
skos:prefLabel	Growth of early continental crust controlled by melting of amphibolite in subduction zones (en) Growth of early continental crust controlled by melting of amphibolite in subduction zones (nl)
name	Growth of early continental crust controlled by melting of amphibolite in subduction zones (en) Growth of early continental crust controlled by melting of amphibolite in subduction zones (nl)
author	wds:Q59059067-0E9B6205-9943-4D78-B359-93B3EABEA1ED wds:Q59059067-743CD7EB-320B-4A6B-B06E-7447B01288C5
author	Massimo Tiepolo Stephen Foley
title	wds:Q59059067-74BA0D24-E9A9-40E1-BC58-F9C204F9074E
title	Growth of early continental crust controlled by melting of amphibolite in subduction zones (en)
page(s)	wds:Q59059067-ABF2FB25-55AB-478A-9FC0-A7A065BDAB09
page(s)	837-840
instance of	wds:Q59059067-AFF98A3F-C97F-48C5-9EFA-8B8D00084CDE
instance of	scholarly article
main subject	wds:Q59059067-D1050E3E-8359-4E6F-8DB8-6BBD6BA3044E
main subject	subduction zone
PubMed ID	wds:Q59059067-FCA41883-864E-4F7C-A824-9CFE4661AF4E
PubMed ID	http://rdf.ncbi.nlm.nih.gov/pubchem/reference/12075348
PubMed ID	12075348
published in	wds:Q59059067-AE674560-D298-42DD-A2D5-0E449EC7C640
published in	Nature
issue	wds:Q59059067-FF2B6F24-E43D-4741-81D6-377FF9F7A99C
volume	wds:Q59059067-0F1A0E1E-006F-421E-901C-1E10F082996E
issue	6891
volume	417
DOI	wds:Q59059067-C7F0F4E7-9DAC-4AC2-B064-E325BF5B0D19
DOI	http://dx.doi.org/10.1038/NATURE00799
DOI	10.1038/NATURE00799
Dimensions Publication ID	wds:Q59059067-443733E6-A3F5-47C7-B603-3AC012CD077F
Dimensions Publication ID	1031298732
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q59059067
is cites work of	Crustal thickness control on Sr/Y signatures of recent arc magmas: an Earth scale perspective Growth of early continental crust by partial melting of eclogite Earth's first stable continents did not form by subduction. Archaean Intracrustal Differentiation from Partial Melting of Metagabbro--Field and Geochemical Evidence from the Central Region of the Lewisian Complex, NW Scotland Delamination and recycling of Archaean crust caused by gravitational instabilities Experimental constraints on TTG petrogenesis: Implications for Archean geodynamics When crust comes of age: on the chemical evolution of Archaean, felsic continental crust by crustal drip tectonics No evidence for high-pressure melting of Earth's crust in the Archean The inception of plate tectonics: a record of failure Petrogenesis of high Ba–Sr plutons with high Sr/Y ratios in an intracontinental setting: evidence from Early Cretaceous Fushan monzonites, central North China Craton Building cratonic keels in Precambrian plate tectonics Geochemical and petrological evidence for subduction–accretion processes in the Archean Eastern Indian Craton Evolution of the Archaean crust by delamination and shallow subduction Geochemical evolution of Monowai volcanic center: New insights into the northern Kermadec arc subduction system, SW Pacific Pargasite at high pressure and temperature The Role of Subducted Basalt in the Source of Island Arc Magmas: Evidence from Seafloor Lavas of the Western Aleutians Source and fractionation controls on subduction-related plutons and dike swarms in southern Patagonia (Torres del Paine area) and the low Nb/Ta of upper crustal igneous rocks. Partial melting of deeply subducted eclogite from the Sulu orogen in China Cyclic formation and stabilization of Archean lithosphere by accretionary orogenesis: Constraints from TTG and potassic granitoids, North China Craton Generation of Archaean TTG Gneisses Through Amphibole‐Dominated Fractionation 10Be, 18O and radiogenic isotopic constraints on the origin of adakitic signatures: a case study from Solander and Little Solander Islands, New Zealand

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