Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Déborah Chavrit"'
Publikováno v:
Reference Module in Earth Systems and Environmental Sciences ISBN: 9780124095489
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ef2b6cd430c6067758911a25a8f2363
https://doi.org/10.1016/b978-0-12-822974-3.00224-x
https://doi.org/10.1016/b978-0-12-822974-3.00224-x
Publikováno v:
Chemical Geology
Chemical Geology, Elsevier, 2019, 520, pp.52-59. ⟨10.1016/j.chemgeo.2019.04.025⟩
Chemical Geology, Elsevier, 2019, 520, pp.52-59. ⟨10.1016/j.chemgeo.2019.04.025⟩
International audience; Extraterrestrial materials have He and Ne isotopic compositions that are distinct from those of the Earth's surface. In order to track the extraterrestrial material accreted onto Earth during the Ediacaran period, we have anal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6f2c1d5e3b59734d2296b83d31f44453
https://hal-insu.archives-ouvertes.fr/insu-02916962/file/S0009254119302086.pdf
https://hal-insu.archives-ouvertes.fr/insu-02916962/file/S0009254119302086.pdf
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, Elsevier, 2016, 436, pp.10-18. ⟨10.1016/j.epsl.2015.12.030⟩
Earth and Planetary Science Letters, Elsevier, 2016, 436, pp.10-18. ⟨10.1016/j.epsl.2015.12.030⟩
Sediments contain interplanetary dust particles (IDPs) carrying extraterrestrial noble gases, such as 3 He, which have previously been used to estimate the IDP accretion flux over time and the duration of past environmental events. However, due to it
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::11a4cf4ad37e117de23d3c2a4a1be688
Publikováno v:
Geochimica et cosmochimica acta 176 (2016): 139–156. doi:10.1016/j.gca.2015.12.013
info:cnr-pdr/source/autori:Broadley M.W [1,2], Ballentine C.J.[3], Chavrit D.[1,4], Dallai L.[5], Burgess R.[1]/titolo:Sedimentary halogens and noble gases within Western Antarctic xenoliths: Implications of extensive volatile recycling to the sub continental lithospheric mantle/doi:10.1016%2Fj.gca.2015.12.013/rivista:Geochimica et cosmochimica acta/anno:2016/pagina_da:139/pagina_a:156/intervallo_pagine:139–156/volume:176
info:cnr-pdr/source/autori:Broadley M.W [1,2], Ballentine C.J.[3], Chavrit D.[1,4], Dallai L.[5], Burgess R.[1]/titolo:Sedimentary halogens and noble gases within Western Antarctic xenoliths: Implications of extensive volatile recycling to the sub continental lithospheric mantle/doi:10.1016%2Fj.gca.2015.12.013/rivista:Geochimica et cosmochimica acta/anno:2016/pagina_da:139/pagina_a:156/intervallo_pagine:139–156/volume:176
Recycling of marine volatiles back into the mantle at subduction zones has a profound, yet poorly constrained impact on the geochemical evolution of the Earth’s mantle. Here we present a combined noble gas and halogen study on mantle xenoliths from
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b11cc7e0348e8c791f7d8b11dc85cf99
http://www.cnr.it/prodotto/i/362606
http://www.cnr.it/prodotto/i/362606