Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Low-energy phase boundary pairs and preferred crystallographic orientations of olivines in nanometer-sized ultrapotassic fluid inclusions of Aykhal diamond. / Hwang, S. L.; Shen, P.; Yui, T. F. и др.
в: Lithos, Том 322, 01.12.2018, стр. 392-404.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Low-energy phase boundary pairs and preferred crystallographic orientations of olivines in nanometer-sized ultrapotassic fluid inclusions of Aykhal diamond
AU - Hwang, S. L.
AU - Shen, P.
AU - Yui, T. F.
AU - Chu, H. T.
AU - Logvinova, A. M.
AU - Sobolev, N. V.
N1 - Publisher Copyright: © 2018 Elsevier B.V.
PY - 2018/12/1
Y1 - 2018/12/1
N2 - The healed internal conjugated cleavages at the core of Aykhal octahedral diamond sample AH2 were decorated with {111}dia-facetted ultrapotassic fluid/melt inclusion pockets containing nanosized graphite, phlogopite and olivine (Fo92) inclusions. These olivines are either rounded in pockets with ample fluid, or facetted by the {111}dia mold in the pockets with a fluid film. Transmission electron microscopy revealed two distinct crystallographic characteristics of olivine inclusions: (1)pronounced crystallographic texture of olivines grouped in specific diamond domain, and (2)frequent parallelism or sub-parallelism of specific low-energy faces of the two phases, mainly (010)ol, {120}ol, (001)ol and {111}dia, {110}dia, {100}dia in the order of decreasing preference, forming prominent (010)ol/{111}dia, (010)ol/{110}dia, (001)ol/{110}dia, {120}ol/{111}dia, and {120}ol/{110}dialow-energy phase boundaries with thin liquid film of 1–2 nm in between. These findings not only testify to the extremely low adhesion energies of olivine-diamond boundary pairs, but also imply that, in the presence of a fluid phase, the interfacial energetics and the energetically favored crystallographic orientations of olivine inclusions in diamond can be controlled simply by the settlement/attachment of low-energy facets of olivine crystals precipitating from the parental fluid upon the low-energy {111}dia or {110}dia surfaces of diamond. Such interfacial energetics control and the resultant low-energy boundary pairs are characteristically distinct from the common topotaxy or epitaxy between oxide/silicate mineral pairs, but are in a sense like the Van der Waals heteroepitaxy in artificial systems.
AB - The healed internal conjugated cleavages at the core of Aykhal octahedral diamond sample AH2 were decorated with {111}dia-facetted ultrapotassic fluid/melt inclusion pockets containing nanosized graphite, phlogopite and olivine (Fo92) inclusions. These olivines are either rounded in pockets with ample fluid, or facetted by the {111}dia mold in the pockets with a fluid film. Transmission electron microscopy revealed two distinct crystallographic characteristics of olivine inclusions: (1)pronounced crystallographic texture of olivines grouped in specific diamond domain, and (2)frequent parallelism or sub-parallelism of specific low-energy faces of the two phases, mainly (010)ol, {120}ol, (001)ol and {111}dia, {110}dia, {100}dia in the order of decreasing preference, forming prominent (010)ol/{111}dia, (010)ol/{110}dia, (001)ol/{110}dia, {120}ol/{111}dia, and {120}ol/{110}dialow-energy phase boundaries with thin liquid film of 1–2 nm in between. These findings not only testify to the extremely low adhesion energies of olivine-diamond boundary pairs, but also imply that, in the presence of a fluid phase, the interfacial energetics and the energetically favored crystallographic orientations of olivine inclusions in diamond can be controlled simply by the settlement/attachment of low-energy facets of olivine crystals precipitating from the parental fluid upon the low-energy {111}dia or {110}dia surfaces of diamond. Such interfacial energetics control and the resultant low-energy boundary pairs are characteristically distinct from the common topotaxy or epitaxy between oxide/silicate mineral pairs, but are in a sense like the Van der Waals heteroepitaxy in artificial systems.
KW - Aykhal diamond
KW - Crystallographic orientation relationship
KW - Crystallographic texture
KW - Low-energy phase boundary pairs
KW - Olivine inclusions
KW - TEM
KW - Ultrapotassic fluid inclusions
KW - SOLID INCLUSIONS
KW - SIBERIAN DIAMONDS
KW - DER-WAALS EPITAXY
KW - GARNET
KW - MANTLE
KW - MINERAL INCLUSIONS
KW - FILMS
KW - GROWTH
KW - MICROCRACKS
KW - INSIGHTS
UR - http://www.scopus.com/inward/record.url?scp=85055899764&partnerID=8YFLogxK
U2 - 10.1016/j.lithos.2018.10.026
DO - 10.1016/j.lithos.2018.10.026
M3 - Article
AN - SCOPUS:85055899764
VL - 322
SP - 392
EP - 404
JO - Lithos
JF - Lithos
SN - 0024-4937
ER -
ID: 17302865