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Byerlee's law : ウィキペディア英語版 | Byerlee's law In rheology, Byerlee's law, also known as Byerlee's friction law〔 〕 states that the shear stress required to slide rock surfaces over one another decreases with normal stress, and becomes nearly independent of rock type.〔 〕 It describes an important property of crustal rock, and can be used to determine when fracturing along a geological fault takes place. == See also ==
* Archie's law * Birch's law * Mohr–Coulomb theory
抄文引用元・出典: フリー百科事典『 ウィキペディア(Wikipedia)』 ■ウィキペディアで「Byerlee's law」の詳細全文を読む
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