Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Comparison of diamonds from the Rassolninskaya depression and modern allyuvial placers of the Krasnovshersky District (Ural region). / Vasilev, E. A.; Klepikov, I. V.; Lukianova, L. I.
в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 147, № 1, 2018, стр. 55-68.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
}
TY - JOUR
T1 - Comparison of diamonds from the Rassolninskaya depression and modern allyuvial placers of the Krasnovshersky District (Ural region)
AU - Vasilev, E. A.
AU - Klepikov, I. V.
AU - Lukianova, L. I.
N1 - Publisher Copyright: © 2018 St. Petersburg Nauka Publishing House. All rights reserved.
PY - 2018
Y1 - 2018
N2 - 336 diamonds from deposits of the Rassol'ninskaya depression and 144 crystals from recent alluvium placers of the Krasnovishersky district were studied by IR absorption and photoluminescence (PL) spectroscopy. It is shown that crystals from the Rassol'ninskaya depression have a close to normal distribution of the nitrogen concentration. The average content of nitrogen is 725 ppm and there were not detected any nitrogen-free crystals. The selection from recent alluvium placers contains 25 % crystals with the nitrogen concentration lesser than 150 ppm and 3 % among them are nitrogen-free crystals. Among crystals from the Rassol'ninskaya depression, there are 12 % of octahedral-shaped, 80 % rhombododecahedral and only one crystal has relicts of cubic faces. The collection from recent placers contains 3 % of cubic crystals, 10 % of individuals with relicts of cubic faces, 16 % of octahedroids and 66 % of dodecahedrons. Alluvium diamonds are often encountered with crescent-shaped fissures, which have been remarked only on a single crystal from the Rassol'ninskaya depression. It has been revealed that among diamonds of alluvium placers up to 95 % crystals contain nitrogen in form of B1 defects. Thus, by morphological and structural-mineralogical features, diamonds from the Rassol'ninskaya depression differ from crystals of the nearest recent alluvium placers, and, secondly, by complex of their characteristics, they may belong to a primary deposits.
AB - 336 diamonds from deposits of the Rassol'ninskaya depression and 144 crystals from recent alluvium placers of the Krasnovishersky district were studied by IR absorption and photoluminescence (PL) spectroscopy. It is shown that crystals from the Rassol'ninskaya depression have a close to normal distribution of the nitrogen concentration. The average content of nitrogen is 725 ppm and there were not detected any nitrogen-free crystals. The selection from recent alluvium placers contains 25 % crystals with the nitrogen concentration lesser than 150 ppm and 3 % among them are nitrogen-free crystals. Among crystals from the Rassol'ninskaya depression, there are 12 % of octahedral-shaped, 80 % rhombododecahedral and only one crystal has relicts of cubic faces. The collection from recent placers contains 3 % of cubic crystals, 10 % of individuals with relicts of cubic faces, 16 % of octahedroids and 66 % of dodecahedrons. Alluvium diamonds are often encountered with crescent-shaped fissures, which have been remarked only on a single crystal from the Rassol'ninskaya depression. It has been revealed that among diamonds of alluvium placers up to 95 % crystals contain nitrogen in form of B1 defects. Thus, by morphological and structural-mineralogical features, diamonds from the Rassol'ninskaya depression differ from crystals of the nearest recent alluvium placers, and, secondly, by complex of their characteristics, they may belong to a primary deposits.
KW - Diamonds
KW - FTIR
KW - Morphology
KW - Photoluminescence
KW - Placer
KW - Rassol'ninskaya depression
KW - The Urals
UR - http://www.scopus.com/inward/record.url?scp=85061080795&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:85061080795
VL - 147
SP - 55
EP - 68
JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА
JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА
SN - 0869-6055
IS - 1
ER -
ID: 86254181