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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MDPI AG
2017-07-01
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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. |
first_indexed | 2024-04-13T08:58:30Z |
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institution | Directory Open Access Journal |
issn | 2073-4352 |
language | English |
last_indexed | 2024-04-13T08:58:30Z |
publishDate | 2017-07-01 |
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series | Crystals |
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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