dc.contributor.author |
Perraki, M |
en |
dc.contributor.author |
Korsakov, AV |
en |
dc.contributor.author |
Smith, DC |
en |
dc.contributor.author |
Mposkos, E |
en |
dc.date.accessioned |
2014-03-01T01:31:44Z |
|
dc.date.available |
2014-03-01T01:31:44Z |
|
dc.date.issued |
2009 |
en |
dc.identifier.issn |
0003-004X |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/19915 |
|
dc.subject |
Diamond |
en |
dc.subject |
Erzgebirge |
en |
dc.subject |
Kokchetav |
en |
dc.subject |
Raman |
en |
dc.subject |
Rhodope Metamorphic Province |
en |
dc.subject |
Uhp metamorphism |
en |
dc.subject.classification |
Geochemistry & Geophysics |
en |
dc.subject.classification |
Mineralogy |
en |
dc.subject.other |
data set |
en |
dc.subject.other |
diamond |
en |
dc.subject.other |
inclusion |
en |
dc.subject.other |
metamorphic rock |
en |
dc.subject.other |
microscopy |
en |
dc.subject.other |
petrography |
en |
dc.subject.other |
Raman spectroscopy |
en |
dc.subject.other |
sample preparation |
en |
dc.subject.other |
terrain |
en |
dc.subject.other |
terrane |
en |
dc.subject.other |
ultrahigh pressure metamorphism |
en |
dc.subject.other |
Asia |
en |
dc.subject.other |
Central Europe |
en |
dc.subject.other |
Eurasia |
en |
dc.subject.other |
Europe |
en |
dc.subject.other |
Germany |
en |
dc.subject.other |
Kazakhstan |
en |
dc.subject.other |
Kokchetav Massif |
en |
dc.subject.other |
Rhodope Mountains |
en |
dc.subject.other |
Southern Europe |
en |
dc.subject.other |
West Asia |
en |
dc.title |
Raman spectroscopic and microscopic criteria for the distinction of microdiamonds in ultrahigh-pressure metamorphic rocks from diamonds in sample preparation materials |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.2138/am.2009.2973 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.2138/am.2009.2973 |
en |
heal.language |
English |
en |
heal.publicationDate |
2009 |
en |
heal.abstract |
Natural diamond from three ultrahigh-pressure metamorphic (UHPM) terranes (Erzgebirge Massif, Germany; Kokchetav Massif, Northern Kazakhstan; Rhodope Metamorphic Province, Greece) and synthetic diamond from cutting and polishing materials (paste, spray, saw blade) were studied by means of optical microscopy and Raman microspectroscopy, to constitute a new petrographic and spectroscopic data set that might be a useful tool for identifying and characterizing metamorphic diamond. Several criteria are established for distinguishing natural microdiamond identified in a rock thin section from the externally introduced ones [i.e., diamond as residual particles (contaminants) from the cutting and polishing material] such as the diamond size, the presence of inclusions, coatings, or coexistent phases and two diamond Raman band parameters, i.e., the Raman shift and the full-width at half maximum height (FWHM). |
en |
heal.publisher |
MINERALOGICAL SOC AMER |
en |
heal.journalName |
American Mineralogist |
en |
dc.identifier.doi |
10.2138/am.2009.2973 |
en |
dc.identifier.isi |
ISI:000265157000014 |
en |
dc.identifier.volume |
94 |
en |
dc.identifier.issue |
4 |
en |
dc.identifier.spage |
546 |
en |
dc.identifier.epage |
556 |
en |