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