An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity

Autor: GUILHERME MALLMANN, RAÚL O.C. FONSECA, ADOLFO B. SILVA

Publikováno v: Anais da Academia Brasileira de Ciências, Vol 86, Iss 4, Pp 1609-1629 (2014)

Subduction zone or arc magmas are known to display a characteristic depletion of High Field Strength Elements (HFSE) relative to other similarly incompatible elements, which can be attributed to the presence of the accessory mineral rutile (TiO2) in

Externí odkaz: https://doaj.org/article/8b30a1289e744490946726749df147d6

An experimental study of the partitioning of trace elements between rutile and silicate melt as a function of oxygen fugacity

Autor: Adolfo B. Silva, Raúl O.C. Fonseca, Guilherme Mallmann

Publikováno v: Anais da Academia Brasileira de Ciências, Volume: 86, Issue: 4, Pages: 1609-1629, Published: 21 OCT 2014
Anais da Academia Brasileira de Ciências, Vol 86, Iss 4, Pp 1609-1629 (2014)
Anais da Academia Brasileira de Ciências v.86 n.4 2014
Anais da Academia Brasileira de Ciências
Academia Brasileira de Ciências (ABC)
instacron:ABC

Subduction zone or arc magmas are known to display a characteristic depletion of High Field Strength Elements (HFSE) relative to other similarly incompatible elements, which can be attributed to the presence of the accessory mineral rutile (TiO2) in

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8598aafce794cbd3396e6211a430ac94
https://pubmed.ncbi.nlm.nih.gov/25590703