砂岩中的孔隙块和应变局部化
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摘要
<正>近些年的研究发现,在高围压条件下,某些特定的砂岩呈现出不一样的破坏模式。这是一种介于脆性和韧性的最终破坏模式,叫做局部化离散压缩带。这是一种平面结构压缩带,垂直于平面方向的缩短导致了平面内的碎裂压缩,伴随着非常少量的剪切。这种压缩带的首次报道见于野外研究中(Hill,1989;Sternlof et al.,2005;Eichhubl et al.,2010),后来在实验室得到了系统的研究(Baud et al.,2004)。研究指出这种现象至少在三种岩石中存在,分别是Bleurswiller砂岩、Diemelstadt砂岩和
引文
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