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An EBSD study of olivine inclusions in Siberian diamonds : Evidence for syngenetic growth? / Neuser, R. D.; Schertl, H. P.; Logvinova, A. M. et al.

In: Russian Geology and Geophysics, Vol. 56, No. 1-2, 01.01.2015, p. 321-329.

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

Harvard

Neuser, RD, Schertl, HP, Logvinova, AM & Sobolev, NV 2015, 'An EBSD study of olivine inclusions in Siberian diamonds: Evidence for syngenetic growth?', Russian Geology and Geophysics, vol. 56, no. 1-2, pp. 321-329. https://doi.org/10.1016/j.rgg.2015.01.023

APA

Neuser, R. D., Schertl, H. P., Logvinova, A. M., & Sobolev, N. V. (2015). An EBSD study of olivine inclusions in Siberian diamonds: Evidence for syngenetic growth? Russian Geology and Geophysics, 56(1-2), 321-329. https://doi.org/10.1016/j.rgg.2015.01.023

Vancouver

Neuser RD, Schertl HP, Logvinova AM, Sobolev NV. An EBSD study of olivine inclusions in Siberian diamonds: Evidence for syngenetic growth? Russian Geology and Geophysics. 2015 Jan 1;56(1-2):321-329. doi: 10.1016/j.rgg.2015.01.023

Author

Neuser, R. D. ; Schertl, H. P. ; Logvinova, A. M. et al. / An EBSD study of olivine inclusions in Siberian diamonds : Evidence for syngenetic growth?. In: Russian Geology and Geophysics. 2015 ; Vol. 56, No. 1-2. pp. 321-329.

BibTeX

@article{3e41c4a88aa742e8848ade7f0d563fee,
title = "An EBSD study of olivine inclusions in Siberian diamonds: Evidence for syngenetic growth?",
abstract = "Crystallographic relations between four diamonds from the Yubileinaya pipe (Yakutia) and inclusions of eight olivine crystals in them are first studied by the EBSD method. Crystallographic coincidence between the olivine and diamond has been revealed in 15 samples, though we failed to make an unambiguous conclusion about the sequence of the mineral crystallization. It is confirmed that the new approach is promising for elucidation of the regularities of the mutual orientation of diamond and inclusion. However, more samples are required to establish whether the olivines formed earlier than the diamonds (protogenetic inclusions) or synchronously with them (syngenetic inclusions).",
keywords = "Back-scattered electron diffraction, Crystallographic relations, Diamond, Olivine",
author = "Neuser, {R. D.} and Schertl, {H. P.} and Logvinova, {A. M.} and Sobolev, {N. V.}",
year = "2015",
month = jan,
day = "1",
doi = "10.1016/j.rgg.2015.01.023",
language = "English",
volume = "56",
pages = "321--329",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "1-2",

}

RIS

TY - JOUR

T1 - An EBSD study of olivine inclusions in Siberian diamonds

T2 - Evidence for syngenetic growth?

AU - Neuser, R. D.

AU - Schertl, H. P.

AU - Logvinova, A. M.

AU - Sobolev, N. V.

PY - 2015/1/1

Y1 - 2015/1/1

N2 - Crystallographic relations between four diamonds from the Yubileinaya pipe (Yakutia) and inclusions of eight olivine crystals in them are first studied by the EBSD method. Crystallographic coincidence between the olivine and diamond has been revealed in 15 samples, though we failed to make an unambiguous conclusion about the sequence of the mineral crystallization. It is confirmed that the new approach is promising for elucidation of the regularities of the mutual orientation of diamond and inclusion. However, more samples are required to establish whether the olivines formed earlier than the diamonds (protogenetic inclusions) or synchronously with them (syngenetic inclusions).

AB - Crystallographic relations between four diamonds from the Yubileinaya pipe (Yakutia) and inclusions of eight olivine crystals in them are first studied by the EBSD method. Crystallographic coincidence between the olivine and diamond has been revealed in 15 samples, though we failed to make an unambiguous conclusion about the sequence of the mineral crystallization. It is confirmed that the new approach is promising for elucidation of the regularities of the mutual orientation of diamond and inclusion. However, more samples are required to establish whether the olivines formed earlier than the diamonds (protogenetic inclusions) or synchronously with them (syngenetic inclusions).

KW - Back-scattered electron diffraction

KW - Crystallographic relations

KW - Diamond

KW - Olivine

UR - http://www.scopus.com/inward/record.url?scp=84925298254&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2015.01.023

DO - 10.1016/j.rgg.2015.01.023

M3 - Article

AN - SCOPUS:84925298254

VL - 56

SP - 321

EP - 329

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 1-2

ER -

ID: 25764104