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Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe : Evidence from the systematics of optically active defects. / Skuzovatov, S. Yu; Zedgenizov, D. A.; Rakevich, A. L. et al.

In: Russian Geology and Geophysics, Vol. 56, No. 1-2, 01.01.2015, p. 330-343.

Research output: Contribution to journal › Article › peer-review

Harvard

Skuzovatov, SY, Zedgenizov, DA, Rakevich, AL, Shatsky, VS & Martynovich, EF 2015, 'Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe: Evidence from the systematics of optically active defects', Russian Geology and Geophysics, vol. 56, no. 1-2, pp. 330-343. https://doi.org/10.1016/j.rgg.2015.01.024

APA

Skuzovatov, S. Y., Zedgenizov, D. A., Rakevich, A. L., Shatsky, V. S., & Martynovich, E. F. (2015). Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe: Evidence from the systematics of optically active defects. Russian Geology and Geophysics, 56(1-2), 330-343. https://doi.org/10.1016/j.rgg.2015.01.024

Vancouver

Skuzovatov SY, Zedgenizov DA, Rakevich AL, Shatsky VS, Martynovich EF. Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe: Evidence from the systematics of optically active defects. Russian Geology and Geophysics. 2015 Jan 1;56(1-2):330-343. doi: 10.1016/j.rgg.2015.01.024

Author

Skuzovatov, S. Yu ; Zedgenizov, D. A. ; Rakevich, A. L. et al. / Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe : Evidence from the systematics of optically active defects. In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 1-2. pp. 330-343.

BibTeX

@article{d4547499cc7341b398b8c867b39a4324,
title = "Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe: Evidence from the systematics of optically active defects",
abstract = "We present new data on the main and additional optically active defects in diamonds with cloudy microinclusions from the Mir kimberlite pipe. It has been found that reshaping might have occurred either in a closed system with nitrogen and hydrogen depletion or owing to new portions of a diamond-forming fluid/melt. The internal structure and the distribution of optically active defects suggest both continuous growth of such diamonds and a multistage scenario with a series of postcrystallizational transformations, including resorption, high-temperature annealing, and degradation of nickel-nitrogen complexes.",
keywords = "Diamond, FTIR spectroscopy, Hydrogen, Nitrogen, Photoluminescence",
author = "Skuzovatov, {S. Yu} and Zedgenizov, {D. A.} and Rakevich, {A. L.} and Shatsky, {V. S.} and Martynovich, {E. F.}",
year = "2015",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2015.01.024",
language = "English",
volume = "56",
pages = "330--343",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1-2",

}

RIS

TY - JOUR

T1 - Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe

T2 - Evidence from the systematics of optically active defects

AU - Skuzovatov, S. Yu

AU - Zedgenizov, D. A.

AU - Rakevich, A. L.

AU - Shatsky, V. S.

AU - Martynovich, E. F.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - We present new data on the main and additional optically active defects in diamonds with cloudy microinclusions from the Mir kimberlite pipe. It has been found that reshaping might have occurred either in a closed system with nitrogen and hydrogen depletion or owing to new portions of a diamond-forming fluid/melt. The internal structure and the distribution of optically active defects suggest both continuous growth of such diamonds and a multistage scenario with a series of postcrystallizational transformations, including resorption, high-temperature annealing, and degradation of nickel-nitrogen complexes.

AB - We present new data on the main and additional optically active defects in diamonds with cloudy microinclusions from the Mir kimberlite pipe. It has been found that reshaping might have occurred either in a closed system with nitrogen and hydrogen depletion or owing to new portions of a diamond-forming fluid/melt. The internal structure and the distribution of optically active defects suggest both continuous growth of such diamonds and a multistage scenario with a series of postcrystallizational transformations, including resorption, high-temperature annealing, and degradation of nickel-nitrogen complexes.

KW - Diamond

KW - FTIR spectroscopy

KW - Hydrogen

KW - Nitrogen

KW - Photoluminescence

UR - http://www.scopus.com/inward/record.url?scp=84925292400&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.01.024

DO - 10.1016/j.rgg.2015.01.024

M3 - Article

AN - SCOPUS:84925292400

VL - 56

SP - 330

EP - 343

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1-2

ER -

ID: 25481692