About: Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos

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About: Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos Goto Sponge NotDistinct Permalink

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rdf:type	Item
description	wetenschappelijk artikel (nl) article scientifique publié en 2016 (fr) наукова стаття, опублікована у вересні 2016 (uk) im September 2016 veröffentlichter wissenschaftlicher Artikel (de)
publication date	wds:Q57887363-C59BE396-6FC2-40FB-954D-C733DDD219D7
publication date	2016-09-05 00:00:00Z (xsd:dateTime)
language of work or name	wds:Q57887363-025AC883-E8CA-456E-8CEF-D523B6871216
language of work or name	English
exact match	wds:Q57887363-FA404601-1C5B-4D6C-8472-A3759FBA7E4D
exact match	https://scigraph.springernature.com/pub.10.1038/ngeo2801
cites work	wds:Q57887363-012C9AB1-CF73-4D37-B0E3-93755C92941B wds:Q57887363-1ADDE758-F8D2-48A1-AC02-EE94B5D35272 wds:Q57887363-1E2DBEBA-10A5-4F4A-AC4C-1456F2463CC9 wds:Q57887363-220B7157-CCF3-4E73-B2F1-B364A1D073A6 wds:Q57887363-23C1DB45-4005-45B4-B4F0-9E9DDAC27572 wds:Q57887363-28CD2460-AE79-471E-BADA-54604558FCD3 wds:Q57887363-334DC64B-9355-460F-BDC9-EC887F4CCD2C wds:Q57887363-33F31FCF-46F5-4FA1-92DF-876F8CD6D3A0 wds:Q57887363-3786EA78-FBAE-4B8B-A797-0536737B9952 wds:Q57887363-43D3B5FD-C344-44D4-B16B-706292F41872 wds:Q57887363-44A9C2FF-39AE-400A-9632-E396CC308C2B wds:Q57887363-48F835F4-E9E1-495D-96F1-53BFDAB891B3 wds:Q57887363-5A21E701-BE12-4DE5-9421-6B08B6ABD42D wds:Q57887363-676E3941-9EAC-4F78-8487-397139737FCB wds:Q57887363-6AC72DA9-7CDE-4F6F-B247-108585BFACC9 wds:Q57887363-6E498527-2C20-4F0C-BAA4-05D13175640A wds:Q57887363-732E5FA8-AE3F-4D4A-9191-5CD6C3B3B837 wds:Q57887363-742BE4EF-9A50-4F2B-A485-2CA46AC16584 wds:Q57887363-7CCA317E-1F9E-4F7B-A977-616DCF81A0F0 wds:Q57887363-87B15420-C88C-4789-B2B3-463B8FC8D55D wds:Q57887363-8899FD54-50D6-430A-9BC1-92ECE2EB2104 wds:Q57887363-97822CA3-E665-47E8-BF01-DA163A8DAE0B wds:Q57887363-9E97C793-55BD-4C56-935E-A7139BF33BA7 wds:Q57887363-B5F817E0-D7EE-4B03-87DE-22CD9E72323D wds:Q57887363-BDE185F7-ECF2-460D-8502-093F7CADDF48 wds:Q57887363-CBA754CC-2A0E-4EE5-8E23-0453DC8979F3 wds:Q57887363-EE68C9D8-022F-41D9-A188-F2B503A28557
cites work	The composition of the Earth CO2 solubility and speciation in rhyolitic sediment partial melts at 1.5–3.0GPa – Implications for carbon flux in subduction zones Melting phase relation of nominally anhydrous, carbonated pelitic-eclogite at 2.5–3.0 GPa and deep cycling of sedimentary carbon Volatile accretion history of the terrestrial planets and dynamic implications Volatile accretion history of the Earth. Carbon solubility in core melts in a shallow magma ocean environment and distribution of carbon between the Earth’s core and the mantle Non-chondritic sulphur isotope composition of the terrestrial mantle Carbon solution and partitioning between metallic and silicate melts in a shallow magma ocean: Implications for the origin and distribution of terrestrial carbon Accretion and differentiation of the terrestrial planets with implications for the compositions of early-formed Solar System bodies and accretion of water Heterogeneous accretion and the moderately volatile element budget of Earth. Ratios of S, Se and Te in the silicate Earth require a volatile-rich late veneer. Effect of pressure, temperature, and oxygen fugacity on the metal-silicate partitioning of Te, Se, and S: Implications for earth differentiation Constraints on the abundance of carbon in near-surface materials on Mercury: Results from the MESSENGER Gamma-Ray Spectrometer Speciation and solubility of reduced C–O–H–N volatiles in mafic melt: Implications for volcanism, atmospheric evolution, and deep volatile cycles in the terrestrial planets Highly reducing conditions during core formation on Mercury: Implications for internal structure and the origin of a magnetic field Copper isotope evidence for large-scale sulphide fractionation during Earth’s differentiation The effects of sulfur, silicon, water, and oxygen fugacity on carbon solubility and partitioning in Fe-rich alloy and silicate melt systems at 3 GPa and 1600 °C: Implications for core–mantle differentiation and degassing of magma oceans and redu Darkening of Mercury's surface by cometary carbon Carbon-bearing iron phases and the carbon isotope composition of the deep Earth Experimental determination of C, F, and H partitioning between mantle minerals and carbonated basalt, CO 2 /Ba and CO 2 /Nb systematics of partial melting, and the CO 2 contents of basaltic source regions Is Mercury a volatile-rich planet? Partitioning of carbon between Fe-rich alloy melt and silicate melt in a magma ocean – Implications for the abundance and origin of volatiles in Earth, Mars, and the Moon Tracing the ingredients for a habitable earth from interstellar space through planet formation A Mercury-like component of early Earth yields uranium in the core and high mantle (142)Nd Effect of carbon, sulfur and silicon on iron melting at high pressure: Implications for composition and evolution of the planetary terrestrial cores Sulfur concentration of martian basalts at sulfide saturation at high pressures and temperatures – Implications for deep sulfur cycle on Mars Carbon-saturated monosulfide melting in the shallow mantle: solubility and effect on solidus
author name string	wds:Q57887363-0C7C8AAD-D334-4F92-9979-05A51A7FAF5B wds:Q57887363-69A1A1BF-7571-4C70-836C-4C2935BF2E4B wds:Q57887363-86FE7412-4CA7-4587-AA1D-5CCC71BB8C21 wds:Q57887363-A013A556-1E4B-461F-BDB0-6BA5A7C5492D
author name string	Yuan Li Kyusei Tsuno Nobumichi Shimizu Brian Monteleone
rdfs:label	Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (en) Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (nl)
skos:prefLabel	Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (en) Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (nl)
name	Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (en) Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (nl)
author	wds:Q57887363-85F56A00-ECAF-479B-86C6-3084A8007E56
author	Rajdeep Dasgupta
title	wds:Q57887363-82103173-3501-4D26-984F-8D21FA06C959
title	Carbon and sulfur budget of the silicate Earth explained by accretion of differentiated planetary embryos (en)
page(s)	wds:Q57887363-4D26E7D8-7F25-4592-9B78-8E76073BFE3E
page(s)	781-785
instance of	wds:Q57887363-EF922A22-5102-413A-AFDC-4A10C682FBE2
instance of	scholarly article
published in	wds:Q57887363-0FB47450-F323-401E-94FD-8A2FE7CC242C
published in	Nature Geoscience
issue	wds:Q57887363-DD494D08-15B0-47CF-811F-A3F6D4615517
volume	wds:Q57887363-C7A38500-E43F-4B64-8A25-3E52819BF137
issue	10
volume	9
DOI	wds:Q57887363-61025DD8-3E47-40FD-8096-52440F04DE85
DOI	http://dx.doi.org/10.1038/NGEO2801
DOI	10.1038/NGEO2801
is about of	https://www.wikidata.org/wiki/Special:EntityData/Q57887363
is cites work of	Rise of Earth’s atmospheric oxygen controlled by efficient subduction of organic carbon CO2 content of andesitic melts at graphite-saturated upper mantle conditions with implications for redox state of oceanic basalt source regions and remobilization of reduced carbon from subducted eclogite Early episodes of high-pressure core formation preserved in plume mantle.

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