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Specific Internal Structure of Diamonds from Zarnitsa Kimberlite Pipe Научная публикация

Журнал Crystals
, E-ISSN: 2073-4352
Вых. Данные Год: 2017, Том: 7, Номер: 5, Номер статьи : 133, Страниц : 10 DOI: 10.3390/cryst7050133
Ключевые слова Diamond; Diffraction of backscattered electrons; Internal structure; Radial mosaic pattern; Zarnitsa kimberlite pipe
Авторы Ragozin Alexey 1,2 , Zedgenizov Dmitry 1,2 , Kuper Konstantin 3 , Palyanov Yuri 1,2
Организации
1 V. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences
2 Department of Geology and Geophysics, Novosibirsk State University
3 Budker Institute of Nuclear Physics, Siberian Branch Russian Academy of Sciences

Реферат: The Zarnitsa kimberlite pipe is one of the largest pipes of the Yakutian diamondiferous province. Currently, some limited published data exists on the diamonds from this deposit. Among the diamond population of this pipe there is a specific series of dark gray to black diamonds with transition morphologies between octahedron and rounded rhombic dodecahedron. These diamonds have specific zonal and sectorial mosaic-block internal structures. The inner parts of these crystals have polycrystalline structure with significant misorientations between sub-individuals. The high consistency of the mechanical admixtures (inclusions) in the diamonds cores can cause a high grid stress of the crystal structure and promote the block (polycrystalline) structure of the core components. These diamond crystals have subsequently been formed due to crystallization of bigger sub-individuals on the polycrystalline cores according to the geometric selection law. © 2017 by the authors. Licensee MDPI, Basel, Switzerland.
Библиографическая ссылка: Ragozin A. , Zedgenizov D. , Kuper K. , Palyanov Y.
Specific Internal Structure of Diamonds from Zarnitsa Kimberlite Pipe
Crystals. 2017. V.7. N5. 133 :1-10. DOI: 10.3390/cryst7050133 WOS Scopus РИНЦ CAPlusCA OpenAlex
Файлы: Полный текст от издателя
Даты:
Поступила в редакцию: 30 мар. 2017 г.
Принята к публикации: 7 мая 2017 г.
Опубликована online: 11 мая 2017 г.
Опубликована в печати: 17 мая 2017 г.
Идентификаторы БД:
Web of science: WOS:000402965400015
Scopus: 2-s2.0-85019268194
РИНЦ: 31033531
Chemical Abstracts: 2017:1185681
Chemical Abstracts (print): 170:493061
OpenAlex: W2613830523
Цитирование в БД:
БД Цитирований
Web of science 7
Scopus 9
OpenAlex 10
Альметрики: