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  1. 100. 学内刊行物 (紀要、研究報告)
  2. 101-3. 奈良教育大学紀要 (人文・社会科学, 自然科学)
  3. 第51巻 第2号 自然科学 (2002)

Stress Effect on Thermoluminescence Intensities of Quartz Grains  ―For the Establishment of a Fault Dating Method―

http://hdl.handle.net/10105/388
http://hdl.handle.net/10105/388
4b62fb8b-d87e-4991-bab6-bb78bb38a208
名前 / ファイル ライセンス アクション
NUE02_02.pdf NUE02_02.pdf (308.6 kB)
アイテムタイプ 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-06-10
タイトル
タイトル Stress Effect on Thermoluminescence Intensities of Quartz Grains  ―For the Establishment of a Fault Dating Method―
言語
言語 eng
キーワード
主題 stress effect, shear fracture, TL fault dating
資源タイプ
資源タイプ departmental bulletin paper
著者 HIRAGA, Shozo

× HIRAGA, Shozo

HIRAGA, Shozo

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MORIMOTO, Akira

× MORIMOTO, Akira

MORIMOTO, Akira

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SHIMAMOTO, Toshihiko

× SHIMAMOTO, Toshihiko

SHIMAMOTO, Toshihiko

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抄録
内容記述タイプ Abstract
内容記述 We have investigated the process of recovery of radiation damages at the time of fault movement, an elementary process attributed to stress, and examined the change of thermoluminescence (TL) intensities of quartz grains with diameters of 1-45 or 45-125 μ m , sheared under a slip rate of 100 μ m /s. The following results were obtained as a result of the experiments. (1) TL intensities increase once with increasing stress, at larger rates for smaller grains. (2) With further increase in stress, the TL intensities peak then revert back to decrease, also at a larger rate for smaller grains. However, this reversion to original TL intensities occurs at higher stress for fine-grained samples. (3) Complete zeroing of TL intensities is not confirmed even at normal stress at ~60 MPa, regardless of grain size. These observations have been interpreted as follows. (1) The increase of TL intensities with increasing stress is due to the so-called radiation damage increment induced by generation of detached electrons at the time of new surface formation caused by shear fracture. (2) The decrease of TL intensities is due to the recovery of damages at the stress where no substantial shear fracture occurs. (3) If a grain-surface phenomenon is responsible for both the increase and the decrease of TL intensities, then the effect is expected to be greater for finer grains, because the surface areas of samples with equal mass are inversely proportional to the radii. The stress effect may not be the only factor contributing to the complete recovery of radiation damages at the time of fault movement. The possibility remains that a complete recovery may be brought about by a rise in temperature due to frictional heating. If the temperature rise were uniform throughout a crush zone, the effect should be independent of grain size, and the complete zeroing of TL intensities should depend only on the degree of temperature rise during fault movement. This is a subject for future studies, to establish a detection method of complete zeroing using the most appropriate TL method for evaluating the thermal hysteresis of samples.
書誌情報 奈良教育大学紀要. 自然科学

巻 51, 号 2, p. 17-24, 発行日 2002-10
ISSN
収録物識別子タイプ ISSN
収録物識別子 05472407
書誌レコードID
収録物識別子タイプ NCID
収録物識別子 AN00181070
著者版フラグ
出版タイプ VoR
出版者
出版者 奈良教育大学
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