Preferred Orientation Evolution of Olivine Grains as an Indicator of Change in the Deformation Mechanism

書誌詳細
Parent link:IOP Conference Series: Materials Science and Engineering
Vol. 91: VI International Scientific Practical Conference on Innovative Technologies and Economics in Engineering, Yurga, Russia, 21-23 May 2015.— 2015.— [012025, 6 p.]
団体著者: Национальный исследовательский Томский политехнический университет (ТПУ) Юргинский технологический институт (филиал) (ЮТИ) Кафедра технологии машиностроения (ТМС)
その他の著者: Lychagin D. V. Dmitry Vasilievich, Tishin P. A., Kulkov A. S., Chernyshov A. I., Alferova (Alfyorova) E. A. Ekaterina Aleksandrovna
要約:Title screen
The paper presents the results of investigations of deformed natural polycrystalline olivine. The relationship of the structure of polycrystalline olivine grains to three modal size distributions has been revealed. Grains of different size were observed to be strained at threshold temperatures of 950, 775, and 650°С. It has been demonstrated that the microstructure develops as the dislocation mechanism changes from diffusion creep to grain boundary sliding. The changes in deformation mechanisms promote the change in the preferred crystallographic orientations of olivine from type A to type D and then to type B. The relation of the transitions between different types of orientations to the conditions of deformation in the lower layers of the lithosphere at the plate boundaries is discussed.
Режим доступа: по договору с организацией-держателем ресурса
言語:英語
出版事項: 2015
シリーズ:Innovative technologies for producing and machining materials in mechanical engineering
主題:
オンライン・アクセス:http://dx.doi.org/10.1088/1757-899X/91/1/012025
http://earchive.tpu.ru/handle/11683/19792
フォーマット: 電子媒体 図書の章
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=644419

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330 |a The paper presents the results of investigations of deformed natural polycrystalline olivine. The relationship of the structure of polycrystalline olivine grains to three modal size distributions has been revealed. Grains of different size were observed to be strained at threshold temperatures of 950, 775, and 650°С. It has been demonstrated that the microstructure develops as the dislocation mechanism changes from diffusion creep to grain boundary sliding. The changes in deformation mechanisms promote the change in the preferred crystallographic orientations of olivine from type A to type D and then to type B. The relation of the transitions between different types of orientations to the conditions of deformation in the lower layers of the lithosphere at the plate boundaries is discussed. 
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701 1 |a Alferova (Alfyorova)  |b E. A.  |c specialist in the field of mechanical engineering  |c associate Professor Yurginsky technological Institute (branch) of Tomsk Polytechnic University, candidate of physical and mathematical Sciences  |f 1982-  |g Ekaterina Aleksandrovna  |2 stltpush  |3 (RuTPU)RU\TPU\pers\34576  |9 17938 
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