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首页> 外文期刊>GSA Bulletin >DEFORMATION OF YULE MARBLE: PART I--COMPRESSION AND EXTENSION EXPERIMENTS ON DRY YULE MARBLE AT 10,000 ATMOSPHERES CONFINING PRESSURE, ROOM TEMPERATURE
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DEFORMATION OF YULE MARBLE: PART I--COMPRESSION AND EXTENSION EXPERIMENTS ON DRY YULE MARBLE AT 10,000 ATMOSPHERES CONFINING PRESSURE, ROOM TEMPERATURE

机译:大理石的变形:第一部分-10,000个大气压下的干燥球形大理石的压缩和拉伸实验,压力,室温

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摘要

A co-operative study of the deformation of marble is described in this series of three papers. Part I deals with the experimental deformation of jacketed cylinders of dry Yule marble, at room temperature and under a confining fluid pressure of 10,000 atmospheres. Cylinders cut parallel, normal, and at 45° to the plane of foliation were homogeneously deformed varying amounts in uniaxial compression and extension. The stress-strain curves show the mechanical anisotropy of the original marble in relation to the fabric anisotropy. Applying the analytical methods of Part II, it is found that Taylor's hypothesis of the deformation of granular aggregates when applied to gliding on planes provides an explanation of the observed mechanical anisotropy. This correlation in turn provides evidence that both twin and translation gliding occur under these experimental conditions and that their relative importance depends on the original fabric and the orientation of the applied stress. Parts II and III describe other evidence which points toward similar conclusions.
机译:在这三篇论文的系列文章中, 描述了对大理石变形的合作研究。第一部分介绍了干燥的圣诞圆大理石的夹套圆柱体在室温 且在10,000个大气压的封闭流体压力下的实验性变形。 圆柱体平行,垂直且与叶面 成45度切割时,在 单轴压缩和延伸过程中均发生了不同程度的均匀变形。应力-应变曲线 表示原始大理石相对于织物各向异性的机械各向异性。应用 第二部分的分析方法,发现泰勒的粒状骨料变形 假设在平面上滑行时提供了观察到的 < / sup>机械各向异性。这种相关性反过来又提供了证据 ,在这些实验性 条件下,双生滑行和平移滑行都发生了,并且它们的相对重要性取决于 原始面料和施加应力的方向。 II和III部分描述了指向相似 结论的其他证据。

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