The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform | Sciact - CRIS-система Института катализа

The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform Научная публикация

Журнал

Crystals
, E-ISSN: 2073-4352

Вых. Данные

Год: 2017, Том: 7, Номер: 8, Номер статьи : 238, Страниц : 12 DOI: 10.3390/cryst7080238

Ключевые слова

diamond; internal structure; electron backscatter diffraction; X-ray topography

Авторы

Ragozin Alexey ^1,2 , Zedgenizov Dmitry ^1,2 , Kuper Konstantin ³ , Kalinina Viktoria ^1,2 , Zemnukhov Alexey ⁴

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
4	JSC Almazy Anabara, Yakutsk

Yellow cuboid diamonds are commonly found in diamondiferous alluvial placers of the Northeastern Siberian platform. The internal structure of these diamonds have been studied by optical microscopy, X-Ray topography (XRT) and electron backscatter diffraction (EBSD) techniques. Most of these crystals have typical resorption features and do not preserve primary growth morphology. The resorption leads to an evolution from an originally cubic shape to a rounded tetrahexahedroid. Specific fibrous or columnar internal structure of yellow cuboid diamonds has been revealed. Most of them are strongly deformed. Misorientations of the crystal lattice, found in the samples, may be caused by strains from their fibrous growth or/and post-growth plastic deformation

Ragozin A. , Zedgenizov D. , Kuper K. , Kalinina V. , Zemnukhov A.
The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform

Crystals. 2017. V.7. N8. 238 :1-12. DOI: 10.3390/cryst7080238 WOS Scopus

Полный текст от издателя

Поступила в редакцию:	30 июн. 2017 г.
Принята к публикации:	28 июл. 2017 г.
Опубликована online:	31 июл. 2017 г.
Опубликована в печати:	1 авг. 2017 г.

Web of science	WOS:000408374200010
Scopus	2-s2.0-85026771539