Show simple item record

dc.contributor.authorFeneyrol, Julien
dc.contributor.authorGiuliani, Gaston
dc.contributor.authorOhnenstetter, Daniel
dc.contributor.authorRondeau, Benjamin
dc.contributor.authorFritsch, Emmanuel
dc.contributor.authorFallick, Anthony E.
dc.contributor.authorIchang’i, Daniel
dc.contributor.authorOmito, Edward
dc.contributor.authorRakotondrazafy, Michel
dc.contributor.authorRanatsenho, Madison
dc.contributor.authorLallier, Florent
dc.date.accessioned2014-12-30T11:42:20Z
dc.date.available2014-12-30T11:42:20Z
dc.date.issued2014
dc.identifier.citationFeneyrol, J., Giuliani, G., Ohnenstetter, D., Rondeau, B., Fritsch, E., Fallick, A. E., ... & Lallier, F. (2014). New typology and origin of tsavorite based on trace-element chemistry. European Journal of Mineralogy, ejm2367_pap_gsw.en_US
dc.identifier.urihttp://eurjmin.geoscienceworld.org/content/early/2014/02/13/0935-1221.2014.0026-2367.abstract
dc.identifier.urihttp://hdl.handle.net/11295/78558
dc.description.abstractNew electron-microprobe analyses of ‘tsavorites’ from the Neoproterozoic Metamorphic Mozambique Belt deposits allow the characterization of green grossular according to its trace-element chemistry (V, Cr, Mn). Five chemical types are defined: type 1, vanadian grossular with V >Cr >Mn (in atoms per formula unit); type 2, vanadian grossular with V >Mn >Cr; type 3, Mn-bearing vanadian grossular with Mn > V > Cr; type 4, Mn-bearing chromian grossular with Mn > Cr > V; and type 5, Cr- and Mn-bearing grossular with Cr > Mn > V. These types are also characterized by different absorption spectra in the ultraviolet–visible–near infrared. Type 1 tsavorite spectra show a total absorption below 430 nm due to the high vanadium contents. Type 2 tsavorite spectra present the classical absorption bands of V. Types 3 and 4 tsavorite spectra display additional shoulders at 407 and 408 nm due to Mn2+, whereas spectra of Cr-bearing types 4 and 5 tsavorite show the two additional bands of Cr3+ at 697 and 701 nm. The different absorption spectra also indicate Fe2+-Ti4+ charge transfer. We measured OH− equivalent to 0.08 to 0.38 wt% eq. H2O within the structure. Concentrations of vanadium, chromium and manganese are good chemical “fingerprints” for determining the geographic provenance of economic tsavorite from Kenya, Tanzania and Madagascar.en_US
dc.language.isoenen_US
dc.publisherUniversity of Nairobien_US
dc.titleNew typology and origin of tsavorite based on trace-element chemistryen_US
dc.typeArticleen_US
dc.type.materialenen_US


Files in this item

Thumbnail

This item appears in the following Collection(s)

Show simple item record