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Diamond-graphite relationships in ultrahigh-pressure metamorphic rocks from the Kokchetav Massif, Northern Kazakhstan

Andrey V Korsakov, Maria Perraki, Dmitry A Zedgenizov, Luca Bindi, Peter Vandenabeele UGent, Akio Suzuki and Hiroyuki Kagi (2010) JOURNAL OF PETROLOGY. 51(3). p.763-783
abstract
Graphite inclusions in diamond, K-bearing clinopyroxene, garnet and kyanite and graphite coatings around microdiamonds from the ultrahigh-pressure Kokchetav Massif, northern Kazakhstan were investigated by means of scanning electron microscopy, laser Raman spectroscopy and X-ray diffraction. Important observations include the increasing size of the graphite crystals from the diamond-graphite interface to the external part of the graphite coatings, the high volume fraction of graphite in the graphite coatings, the presence of composite crystals of successively formed diamond core-graphite mantle zone-diamond rim-external graphite coating, the spherulitic texture of the graphite coatings, the formation of both ordered and disordered graphite and the absence of any fluid associated with the graphite inclusions in diamond and other ultrahigh-pressure metamorphic (UHPM) minerals. These features combined with the presence of oriented graphite flakes in K-bearing clinopyroxene and in diamond-bearing garnet and kyanite and the presence of intergranular diamonds without graphite coatings in the quartzo-feldspathic matrix require reconsideration of the generally accepted diamond graphitization model for interpreting the formation of graphite in UHPM rocks. Metastable growth of graphite within the diamond stability field is suggested and the following crystallization scheme for the C-polymorph is proposed: graphite was the first C-polymorph formed in the diamond stability field, followed by diamond; the graphite coatings around diamond formed during the final stage of UHPM conditions.
Please use this url to cite or link to this publication:
author
organization
year
type
journalArticle (original)
publication status
published
subject
keyword
Raman spectroscopy, Kokchetav Massif, UHP metamorphism, diamond, metastable growth, graphite
journal title
JOURNAL OF PETROLOGY
J. Petrol.
volume
51
issue
3
pages
763 - 783
Web of Science type
Review
Web of Science id
000274500700007
JCR category
GEOCHEMISTRY & GEOPHYSICS
JCR impact factor
3.842 (2010)
JCR rank
5/77 (2010)
JCR quartile
1 (2010)
ISSN
0022-3530
DOI
10.1093/petrology/egq001
language
English
UGent publication?
yes
classification
A1
copyright statement
I have transferred the copyright for this publication to the publisher
id
886454
handle
http://hdl.handle.net/1854/LU-886454
date created
2010-03-02 13:13:57
date last changed
2015-06-17 11:23:10
@article{886454,
  abstract     = {Graphite inclusions in diamond, K-bearing clinopyroxene, garnet and kyanite and graphite coatings around microdiamonds from the ultrahigh-pressure Kokchetav Massif, northern Kazakhstan were investigated by means of scanning electron microscopy, laser Raman spectroscopy and X-ray diffraction. Important observations include the increasing size of the graphite crystals from the diamond-graphite interface to the external part of the graphite coatings, the high volume fraction of graphite in the graphite coatings, the presence of composite crystals of successively formed diamond core-graphite mantle zone-diamond rim-external graphite coating, the spherulitic texture of the graphite coatings, the formation of both ordered and disordered graphite and the absence of any fluid associated with the graphite inclusions in diamond and other ultrahigh-pressure metamorphic (UHPM) minerals. These features combined with the presence of oriented graphite flakes in K-bearing clinopyroxene and in diamond-bearing garnet and kyanite and the presence of intergranular diamonds without graphite coatings in the quartzo-feldspathic matrix require reconsideration of the generally accepted diamond graphitization model for interpreting the formation of graphite in UHPM rocks. Metastable growth of graphite within the diamond stability field is suggested and the following crystallization scheme for the C-polymorph is proposed: graphite was the first C-polymorph formed in the diamond stability field, followed by diamond; the graphite coatings around diamond formed during the final stage of UHPM conditions.},
  author       = {Korsakov, Andrey V and Perraki, Maria and Zedgenizov, Dmitry A and Bindi, Luca and Vandenabeele, Peter and Suzuki, Akio and Kagi, Hiroyuki},
  issn         = {0022-3530},
  journal      = {JOURNAL OF PETROLOGY},
  keyword      = {Raman spectroscopy,Kokchetav Massif,UHP metamorphism,diamond,metastable growth,graphite},
  language     = {eng},
  number       = {3},
  pages        = {763--783},
  title        = {Diamond-graphite relationships in ultrahigh-pressure metamorphic rocks from the Kokchetav Massif, Northern Kazakhstan},
  url          = {http://dx.doi.org/10.1093/petrology/egq001},
  volume       = {51},
  year         = {2010},
}

Chicago
Korsakov, Andrey V, Maria Perraki, Dmitry A Zedgenizov, Luca Bindi, Peter Vandenabeele, Akio Suzuki, and Hiroyuki Kagi. 2010. “Diamond-graphite Relationships in Ultrahigh-pressure Metamorphic Rocks from the Kokchetav Massif, Northern Kazakhstan.” Journal of Petrology 51 (3): 763–783.
APA
Korsakov, A. V., Perraki, M., Zedgenizov, D. A., Bindi, L., Vandenabeele, P., Suzuki, A., & Kagi, H. (2010). Diamond-graphite relationships in ultrahigh-pressure metamorphic rocks from the Kokchetav Massif, Northern Kazakhstan. JOURNAL OF PETROLOGY, 51(3), 763–783.
Vancouver
1.
Korsakov AV, Perraki M, Zedgenizov DA, Bindi L, Vandenabeele P, Suzuki A, et al. Diamond-graphite relationships in ultrahigh-pressure metamorphic rocks from the Kokchetav Massif, Northern Kazakhstan. JOURNAL OF PETROLOGY. 2010;51(3):763–83.
MLA
Korsakov, Andrey V, Maria Perraki, Dmitry A Zedgenizov, et al. “Diamond-graphite Relationships in Ultrahigh-pressure Metamorphic Rocks from the Kokchetav Massif, Northern Kazakhstan.” JOURNAL OF PETROLOGY 51.3 (2010): 763–783. Print.