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

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...

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Main Authors: Alexey Ragozin, Dmitry Zedgenizov, Konstantin Kuper, Viktoria Kalinina, Alexey Zemnukhov
Format: Article
Language:English
Published: MDPI AG 2017-07-01
Series:Crystals
Subjects:
Online Access:https://www.mdpi.com/2073-4352/7/8/238
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author Alexey Ragozin
Dmitry Zedgenizov
Konstantin Kuper
Viktoria Kalinina
Alexey Zemnukhov
author_facet Alexey Ragozin
Dmitry Zedgenizov
Konstantin Kuper
Viktoria Kalinina
Alexey Zemnukhov
author_sort Alexey Ragozin
collection DOAJ
description 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.
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spelling doaj.art-374e4ded9c1b4516a26d1180f0c361a42022-12-22T02:53:11ZengMDPI AGCrystals2073-43522017-07-017823810.3390/cryst7080238cryst7080238The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian PlatformAlexey Ragozin0Dmitry Zedgenizov1Konstantin Kuper2Viktoria Kalinina3Alexey Zemnukhov4V. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences, Novosibirsk 630090, RussiaV. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences, Novosibirsk 630090, RussiaBudker Institute of Nuclear Physics, Siberian Branch Russian Academy of Sciences, Novosibirsk 630090, RussiaV. S. Sobolev Institute of Geology and Mineralogy, Siberian Branch Russian Academy of Sciences, Novosibirsk 630090, RussiaJSC Almazy Anabara, Yakutsk 678174, RussiaYellow 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.https://www.mdpi.com/2073-4352/7/8/238diamondinternal structureelectron backscatter diffractionX-ray topography
spellingShingle Alexey Ragozin
Dmitry Zedgenizov
Konstantin Kuper
Viktoria Kalinina
Alexey Zemnukhov
The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
Crystals
diamond
internal structure
electron backscatter diffraction
X-ray topography
title The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
title_full The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
title_fullStr The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
title_full_unstemmed The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
title_short The Internal Structure of Yellow Cuboid Diamonds from Alluvial Placers of the Northeastern Siberian Platform
title_sort internal structure of yellow cuboid diamonds from alluvial placers of the northeastern siberian platform
topic diamond
internal structure
electron backscatter diffraction
X-ray topography
url https://www.mdpi.com/2073-4352/7/8/238
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