About: Xenon isotopic constraints on the history of volatile recycling into the mantle

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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) scientific article published in Nature (en) im August 2018 veröffentlichter wissenschaftlicher Artikel (de) наукова стаття, опублікована в Nature в серпні 2018 (uk)
publication date	wds:Q59054647-84FE5304-DC89-4401-A7F5-0AE3177E525A
publication date	2018-08-08 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q59054647-CC6BE001-B21F-451C-84BD-C8E3CCA01DF8
language of work or name	English
exact match	wds:Q59054647-93C349B3-6C85-46B8-AB77-79A3F9332F55
exact match	https://scigraph.springernature.com/pub.10.1038/s41586-018-0388-4
cites work	wds:Q59054647-175A71FA-2A1D-4CDF-8EB0-28E759A9497C wds:Q59054647-1ED1CEA1-2AC9-4CFB-8489-430CD31E5025 wds:Q59054647-219F8EE0-91E7-4C11-B43D-1E9AF76A21CD wds:Q59054647-2DDB61C1-0787-4F8E-AD3A-280EFEB1A335 wds:Q59054647-2EA1A133-0BD8-4248-8B93-DBC9B93BEE65 wds:Q59054647-34DB33CC-D52F-47F4-B6B0-16ABFDE98093 wds:Q59054647-3BBBF71C-3D26-4701-8F53-59880D6D65E7 wds:Q59054647-3D4E4D65-AFBA-48EF-A007-034F145AF8B3 wds:Q59054647-4D175C60-53F7-40C6-81E6-A47CA18B3330 wds:Q59054647-5AE805F1-F4FD-41EE-9246-57EC9B84B36F wds:Q59054647-5C196352-CD7A-49F9-95BC-32C098DA80EC wds:Q59054647-6244ACFE-174A-4555-9CD8-8B56B71DB899 wds:Q59054647-73A57334-61B1-43BA-B5E2-F594256F7C8E wds:Q59054647-74EA9279-326E-49C7-8BAE-39C9F6A8DA32 wds:Q59054647-7AA1A89C-FDAF-450C-93D0-707D85011B90 wds:Q59054647-85370C6F-8076-4036-B3C5-260DAEC78363 wds:Q59054647-873E7900-4AEF-4175-B48C-6F701844FAC5 wds:Q59054647-977B4556-D86D-4B1C-9C55-BF0368C0EF91 wds:Q59054647-9C91180D-855C-4F58-A062-68D5A9C717FE wds:Q59054647-A1F2BC7E-3048-4D3C-AE79-4FE30DAA673D wds:Q59054647-A609D7F6-E449-4C72-A2AD-5DE05D6F91EA wds:Q59054647-A9F6B77B-CD06-47C2-B5E6-22EF61BF6BDF wds:Q59054647-AD9ABBE4-9295-436A-AFAF-5E1FED42D357 wds:Q59054647-C7492F5D-B918-4572-BB76-851CAD0F2ADD wds:Q59054647-CBB22C66-00F2-4F6D-A078-EE98BE1C2BB0 wds:Q59054647-E993C101-B54C-4BD6-BE8A-687A235FABB5 wds:Q59054647-F23E559F-AA23-4395-8CCE-94E259160126 wds:Q59054647-F7DD2636-B789-42D8-AB27-1F8126F2A441 wds:Q59054647-FA45F522-5216-45F3-87B5-84A9BB023F6E
cites work	The composition of the Earth Global correlations of ocean ridge basalt chemistry with axial depth and crustal thickness H2O subduction beyond arcs Composition of the Continental Crust Subduction factory: 4. Depth-dependent flux of H2O from subducting slabs worldwide The chemical composition of subducting sediment and its consequences for the crust and mantle Low heat flow inferred from >4 Gyr zircons suggests Hadean plate boundary interactions. Noble gas transport into the mantle facilitated by high solubility in amphibole On the origin and early evolution of terrestrial planet atmospheres and meteoritic volatiles Global water cycle and the coevolution of the Earth's interior and surface environment Start of the Wilson cycle at 3 Ga shown by diamonds from subcontinental mantle Rates of magma emplacement and volcanic output Early differentiation and volatile accretion recorded in deep-mantle neon and xenon Plutonium-244: confirmation as an extinct radioactivity The origin and degassing history of the Earth's atmosphere revealed by Archean xenon Argon isotopic composition of Archaean atmosphere probes early Earth geodynamics Chondritic xenon in the Earth's mantle Quantifying He fluxes from the mantle using multi-tracer data assimilation A change in the geodynamics of continental growth 3 billion years ago. Experimentally based water budgets for dehydrating slabs and consequences for arc magma generation Xenon in Archean barite: Weak decay of 130Ba, mass-dependent isotopic fractionation and implication for barite formation Deep fracture fluids isolated in the crust since the Precambrian era. Duality of thermal regimes is the distinctive characteristic of plate tectonics since the Neoarchean Rare gas systematics in popping rock: isotopic and elemental compositions in the upper mantle Seawater subduction controls the heavy noble gas composition of the mantle Subduction zone fluxes of halogens and noble gases in seafloor and forearc serpentinites High abundances of noble gas and chlorine delivered to the mantle by serpentinite subduction Primordial Noble Gases from Earth's Mantle: Identification of a Primitive Volatile Component Low helium flux from the mantle inferred from simulations of oceanic helium isotope data
author name string	wds:Q59054647-3EA88595-AD87-41D9-A280-3E28E0DC2807
author name string	Sujoy Mukhopadhyay
rdfs:label	Xenon isotopic constraints on the history of volatile recycling into the mantle (en) Xenon isotopic constraints on the history of volatile recycling into the mantle (nl)
skos:prefLabel	Xenon isotopic constraints on the history of volatile recycling into the mantle (en) Xenon isotopic constraints on the history of volatile recycling into the mantle (nl)
name	Xenon isotopic constraints on the history of volatile recycling into the mantle (en) Xenon isotopic constraints on the history of volatile recycling into the mantle (nl)
author	wds:Q59054647-B55E287C-43FE-49D2-B0D5-DCA400D56CE0
author	Rita Parai
title	wds:Q59054647-345FE356-559D-41E2-8CF8-AAED9004C734
title	Xenon isotopic constraints on the history of volatile recycling into the mantle (en)
page(s)	wds:Q59054647-A82FA763-4B12-4EA0-ACBD-D5F13ED61FA0
page(s)	223-227
instance of	wds:Q59054647-E8F6D980-01F4-4739-942D-2A29C6DB7CB4
instance of	scholarly article
main subject	wds:Q59054647-C2DB6F99-B15D-40DE-A88A-79B02D2DBFC1
main subject	wd:Q1106
PubMed ID	wds:Q59054647-66857A01-46AD-464B-AFBA-334E620FE1CF
PubMed ID	http://rdf.ncbi.nlm.nih.gov/pubchem/reference/30089920
PubMed ID	30089920
published in	wds:Q59054647-D7C4F294-B7AE-46D8-95DC-F5E038489A77
published in	Nature
issue	wds:Q59054647-5F0B8C61-05F0-4D16-BF69-6CC42D3F6415
volume	wds:Q59054647-4FFE47D1-B454-4A70-9E7D-2A06558E4A3F
issue	7717
volume	560
DOI	wds:Q59054647-1E98E577-60E0-4909-BAF2-5E5C612219BA
DOI	http://dx.doi.org/10.1038/S41586-018-0388-4

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