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The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform. / Ragozin, Alexey; Zedgenizov, Dmitry; Kuper, Konstantin et al.

In: Crystals, Vol. 7, No. 8, 238, 01.08.2017.

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

Harvard

Ragozin, A, Zedgenizov, D, Kuper, K, Kalinina, V & Zemnukhov, A 2017, 'The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform', Crystals, vol. 7, no. 8, 238. https://doi.org/10.3390/cryst7080238

APA

Ragozin, A., Zedgenizov, D., Kuper, K., Kalinina, V., & Zemnukhov, A. (2017). The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform. Crystals, 7(8), [238]. https://doi.org/10.3390/cryst7080238

Vancouver

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 Aug 1;7(8):238. doi: 10.3390/cryst7080238

Author

Ragozin, Alexey ; Zedgenizov, Dmitry ; Kuper, Konstantin et al. / The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform. In: Crystals. 2017 ; Vol. 7, No. 8.

BibTeX

@article{3744abe4e81745cb9b76df5cdecbaad5,
title = "The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform",
abstract = "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.",
keywords = "Diamond, Electron backscatter diffraction, Internal structure, X-ray topography, CRYSTALLIZATION, ELECTRON BACKSCATTER DIFFRACTION, POLYGENESIS, INCLUSIONS, GROWTH ENVIRONMENT, NATURAL DIAMONDS, diamond, internal structure, DISSOLUTION, CRYSTALS, BIREFRINGENCE, electron backscatter diffraction, MORPHOLOGY",
author = "Alexey Ragozin and Dmitry Zedgenizov and Konstantin Kuper and Viktoria Kalinina and Alexey Zemnukhov",
year = "2017",
month = aug,
day = "1",
doi = "10.3390/cryst7080238",
language = "English",
volume = "7",
journal = "Crystals",
issn = "2073-4352",
publisher = "Multidisciplinary Digital Publishing Institute (MDPI)",
number = "8",

}

RIS

TY - JOUR

T1 - The internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform

AU - Ragozin, Alexey

AU - Zedgenizov, Dmitry

AU - Kuper, Konstantin

AU - Kalinina, Viktoria

AU - Zemnukhov, Alexey

PY - 2017/8/1

Y1 - 2017/8/1

N2 - 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.

AB - 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.

KW - Diamond

KW - Electron backscatter diffraction

KW - Internal structure

KW - X-ray topography

KW - CRYSTALLIZATION

KW - ELECTRON BACKSCATTER DIFFRACTION

KW - POLYGENESIS

KW - INCLUSIONS

KW - GROWTH ENVIRONMENT

KW - NATURAL DIAMONDS

KW - diamond

KW - internal structure

KW - DISSOLUTION

KW - CRYSTALS

KW - BIREFRINGENCE

KW - electron backscatter diffraction

KW - MORPHOLOGY

UR - http://www.scopus.com/inward/record.url?scp=85026771539&partnerID=8YFLogxK

U2 - 10.3390/cryst7080238

DO - 10.3390/cryst7080238

M3 - Article

AN - SCOPUS:85026771539

VL - 7

JO - Crystals

JF - Crystals

SN - 2073-4352

IS - 8

M1 - 238

ER -

ID: 10068890