2011 Fiscal Year Final Research Report
Mechanisms of subgrain boundary development and grain size decrease in mylonite
Project/Area Number |
21540501
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Research Category |
Grant-in-Aid for Scientific Research (C)
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Allocation Type | Single-year Grants |
Section | 一般 |
Research Field |
Petrology/Mineralogy/Science of ore deposit
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Research Institution | Japan Agency for Marine-Earth Science and Technology |
Principal Investigator |
RAIMBOURG Hugues 独立行政法人海洋研究開発機構, 地球内部ダイナミクス領域, 招聘研究員 (40509709)
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Co-Investigator(Kenkyū-buntansha) |
KOGURE Toshihiro 東京大学, 大学院・理学研究科, 准教授 (50282728)
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Project Period (FY) |
2009 – 2011
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Keywords | 岩石変形 / マイロナイト / 細粒化 / 粒界 / 斜方輝石 / TEM / EBSD / FIB |
Research Abstract |
The deformation structures of orthopyroxene(Opx) in mylonite rock from Hidaka Metamorphic belt have been investigated mainly using transmission electron microscopy(TEM). Low-angle grain boundaries with the b-axis as the rotation axes and almost parallel to the(001) plane of Opx are common and their atomic structure are varied from coherent to semi-coherent and finally incoherent, depending on the misorientation angle of the boundaries. Asymmetric misfit dislocation densities along the two(100) interfaces between exsolved augite lamella and host Opx were also found, which is probably the origin of the folding of the Opx crystal.
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Research Products
(8 results)
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[Presentation] Structure Nanoanalyses of Specified Regions in Minerals, Rocks and Soils through SEM-FIB-TEM Sequence2010
Author(s)
Kogure, T., Kameda, J., Beaufort, D., and Raimbourg, H.
Organizer
17th IFSM, International Microscopy Congress
Place of Presentation
Rio de Janeiro, Brazil
Year and Date
2010-09-21