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タイトル: | The role of porosity evolution and fluid flow in frictional instabilities: A parametric study using a spring-slider dynamic system |
著者: | Mitsui, Yuta Cocco, Massimo |
著者名の別形: | 三井, 雄太 |
キーワード: | porosity evolution pore fluid pressure frictional instability fluid flow fault thickness |
発行日: | Dec-2010 |
出版者: | American Geophysical Union |
誌名: | Geophysical Research Letters |
巻: | 37 |
論文番号: | L23305 |
抄録: | We have investigated the role of porosity evolution and fluid flow in frictional instabilities by analyzing the response of a single degree of freedom dynamic system. The spring slider is governed by rate- and state-dependent constitutive law. We also account for effective normal stress changes caused by thermal pressurization with constant or variable porosity. Our simulations show that the stress drop during dynamic instabilities depends on constitutive parameters, porosity evolution, fluid flow as well as on the effective fault zone thickness, defined in this study as the ratio between the nominal thickness of the fault zone (w) and the hydraulically activated layer (why). Both porosity evolution and fluid flow can avoid the extremely large stress drop values inferred by thermal pressurization models and provide an attempt to reconcile them with seismological observations. |
著作権等: | © 2010 by the American Geophysical Union. This is not the published version. Please cite only the published version. この論文は出版社版でありません。引用の際には出版社版をご確認ご利用ください。 |
URI: | http://hdl.handle.net/2433/134563 |
DOI(出版社版): | 10.1029/2010GL045672 |
出現コレクション: | 学術雑誌掲載論文等 |
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