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Impact shock origin of diamonds in ureilite meteorites

Autor: Nestola F.[1, Goodrich C.A.[3], Morana M.[4], Barbaro A.[4], Jakubek R.S.[5], Christ O.[1], Brenker F.E.[2], Domeneghetti M.C.[4], Dalconi M.C.[1], Alvaro M.[4], Fioretti A.M.[6], Litasov K.D.[7], Fries M.D.[8], Leoni M.[9, 10], Casati N.P.M.[11], Jenniskens P.[12], Shaddad M.H.[13]

Publikováno v: Proceedings of the National Academy of Sciences of the United States of America
Proceedings of the National Academy of Sciences of the United States of America 117 (2020): 25310–25318. doi:10.1073/pnas.1919067117
info:cnr-pdr/source/autori:Nestola F.[1,2],Goodrich C.A.[3], Morana M.[4], Barbaro A.[4], Jakubek R.S.[5], Christ O.[1], Brenker F.E.[2], Domeneghetti M.C.[4], Dalconi M.C.[1], Alvaro M.[4], Fioretti A.M.[6], Litasov K.D.[7], Fries M.D.[8], Leoni M.[9,10], Casati N.P.M.[11], Jenniskens P.[12], Shaddad M.H.[13]/titolo:Impact shock origin of diamonds in ureilite meteorites/doi:10.1073%2Fpnas.1919067117/rivista:Proceedings of the National Academy of Sciences of the United States of America/anno:2020/pagina_da:25310/pagina_a:25318/intervallo_pagine:25310–25318/volume:117

Significance The origin of diamonds in ureilites is still a debated issue among the scientific community, with significant implications for the sizes of early Solar System bodies. We investigated three diamond-bearing ureilites by a multimethodologic

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::570a9aa4d3f6e8f049d862dd3831e85d
http://europepmc.org/articles/PMC7568235

Graphite-based geothermometry on almahata sitta ureilitic meteorites

Autor: Barbaro A.[1], Domeneghetti M.C.[1], Goodrich C.A.[2], Meneghetti M.[3], Litti L.[3], Fioretti A.M.[4], Jenniskens P.[5], Shaddad M.H.[6], Nestola F.[7

Publikováno v: Minerals
Volume 10
Issue 11
Minerals (Basel) 10 (2020): 1–14. doi:10.3390/min10111005
info:cnr-pdr/source/autori:Barbaro A.[1], Domeneghetti M.C.[1], Goodrich C.A.[2], Meneghetti M.[3], Litti L.[3], Fioretti A.M.[4], Jenniskens P.[5], Shaddad M.H.[6], Nestola F.[7,8]/titolo:Graphite-based geothermometry on almahata sitta ureilitic meteorites/doi:10.3390%2Fmin10111005/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:14/intervallo_pagine:1–14/volume:10
Minerals, Vol 10, Iss 1005, p 1005 (2020)
Minerals (Basel, Switzerland)

The thermal history of carbon phases, including graphite and diamond, in the ureilite meteorites has implications for the formation, igneous evolution, and impact disruption of their parent body early in the history of the Solar System. Geothermometr

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5e29dbb8c9112d9608f51a293d99d102
http://hdl.handle.net/11577/3364156

Zircon megacrysts from basalts of the Venetian Volcanic Province (NE Italy): U–Pb ages, oxygen isotopes and REE data

Autor: Visonà, D., Caironi, V., Carraro, A., Dallai, L., Fioretti, A.M., Fanning, M.

Publikováno v: In LITHOS 2007 94(1):168-180

High-Nb hawaiite-mugearite and high-Mg calc-alkaline lavas from northeastern Iran: Oligo-Miocene melts from modified mantle wedge

Autor: Ahmadi P.[1], Ghorban M.R.[1], Coltorti M.[2], Kuritani T.[3], Cai Y.[4], Fioretti A.M.[5], Braschi E.[6], Giacomoni P.P.[2], Aghabazaz F.[1], Babazadeh S.[1], Conticelli S.[6

Publikováno v: International geology review 61 (2019): 150–174. doi:10.1080/00206814.2017.1416502
info:cnr-pdr/source/autori:Ahmadi P.[1], Ghorban M.R.[1], Coltorti M.[2], Kuritani T.[3], Cai Y.[4], Fioretti A.M.[5], Braschi E.[6], Giacomoni P.P.[2], Aghabazaz F.[1], Babazadeh S.[1], Conticelli S.[6,7]/titolo:High-Nb hawaiite-mugearite and high-Mg calc-alkaline lavas from northeastern Iran: Oligo-Miocene melts from modified mantle wedge/doi:10.1080%2F00206814.2017.1416502/rivista:International geology review/anno:2019/pagina_da:150/pagina_a:174/intervallo_pagine:150–174/volume:61

Tertiary volcanic rocks in northwestern Firoozeh, Iran (the Meshkan triangular structural unit), constitute vast outcrops (up to 250 km2) of high-Mg basaltic andesites to dacites that are associated with high-Nb hawaiites and mugearites. Whole-rock 4

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c671264d12a1db044ae948aecb513fe8
http://hdl.handle.net/11392/2383180