dc.contributor.author |
Korsakov, AV |
en |
dc.contributor.author |
Vandenabeele, P |
en |
dc.contributor.author |
Perraki, M |
en |
dc.contributor.author |
Moens, L |
en |
dc.date.accessioned |
2014-03-01T02:47:21Z |
|
dc.date.available |
2014-03-01T02:47:21Z |
|
dc.date.issued |
2011 |
en |
dc.identifier.issn |
1386-1425 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/33099 |
|
dc.subject |
Aragonite |
en |
dc.subject |
Calcite |
en |
dc.subject |
Cathodoluminescence |
en |
dc.subject |
Diamond |
en |
dc.subject |
Raman spectroscopy |
en |
dc.subject |
SEM |
en |
dc.subject |
UHPM petrology |
en |
dc.subject.classification |
Spectroscopy |
en |
dc.subject.other |
Aragonite |
en |
dc.subject.other |
Kazakhstan |
en |
dc.subject.other |
Kokchetav massif |
en |
dc.subject.other |
Metamorphic conditions |
en |
dc.subject.other |
Monocrystalline |
en |
dc.subject.other |
Raman analysis |
en |
dc.subject.other |
Raman bands |
en |
dc.subject.other |
Residual pressures |
en |
dc.subject.other |
UHPM petrology |
en |
dc.subject.other |
Carbonate minerals |
en |
dc.subject.other |
Diamonds |
en |
dc.subject.other |
Garnets |
en |
dc.subject.other |
Grain boundaries |
en |
dc.subject.other |
Metamorphic rocks |
en |
dc.subject.other |
Petrography |
en |
dc.subject.other |
Raman spectroscopy |
en |
dc.subject.other |
Rocks |
en |
dc.subject.other |
Single crystals |
en |
dc.subject.other |
Diamond deposits |
en |
dc.subject.other |
calcium carbonate |
en |
dc.subject.other |
diamond |
en |
dc.subject.other |
mineral |
en |
dc.subject.other |
chemistry |
en |
dc.subject.other |
conference paper |
en |
dc.subject.other |
crystallization |
en |
dc.subject.other |
Kazakhstan |
en |
dc.subject.other |
methodology |
en |
dc.subject.other |
Raman spectrometry |
en |
dc.subject.other |
Calcium Carbonate |
en |
dc.subject.other |
Crystallization |
en |
dc.subject.other |
Diamond |
en |
dc.subject.other |
Kazakhstan |
en |
dc.subject.other |
Minerals |
en |
dc.subject.other |
Spectrum Analysis, Raman |
en |
dc.title |
First findings of monocrystalline aragonite inclusions in garnet from diamond-grade UHPM rocks (Kokchetav Massif, Northern Kazakhstan) |
en |
heal.type |
conferenceItem |
en |
heal.identifier.primary |
10.1016/j.saa.2010.12.024 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1016/j.saa.2010.12.024 |
en |
heal.language |
English |
en |
heal.publicationDate |
2011 |
en |
heal.abstract |
The presence of aragonite inclusions in garnet from diamond-grade metamorphic rocks from the Kokchetav Massif, Northern Kazakhstan was identified for the first time by means of Raman analyses and mapping. Aragonite appears within the inclusions up to 50 mu m in size as a single crystal. These inclusions have rounded shape. The grain boundary between the host-garnet is smooth. No cracks occur around the aragonite inclusions. No significant shift in the main aragonite Raman band was measured. These observations indicate that residual pressure within the inclusion is minor. These findings imply either non-UHPM origin of the host garnet or significant plastic deformation of host minerals during retrograde stage. These features should be taken into account for recovery peak metamorphic conditions and modeling of exhumation processes of UHPM complexes. (C) 2010 Elsevier B.V. All rights reserved. |
en |
heal.publisher |
PERGAMON-ELSEVIER SCIENCE LTD |
en |
heal.journalName |
Spectrochimica Acta - Part A: Molecular and Biomolecular Spectroscopy |
en |
dc.identifier.doi |
10.1016/j.saa.2010.12.024 |
en |
dc.identifier.isi |
ISI:000295297900005 |
en |
dc.identifier.volume |
80 |
en |
dc.identifier.issue |
1 |
en |
dc.identifier.spage |
21 |
en |
dc.identifier.epage |
26 |
en |