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Determination of rock stress by anelastic strain recovery measurement of an oriented core in the Nittsu region of Japan

机译:日本Nittsu地区的Anelast resy恢复测量岩体应力测定

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Anelastic strain recovery (ASR) of an oriented andesite core taken from a depth of 4500m MD in a deep well was measured in six independent directions. The recovered anelastic strains were used for a three-dimensional analysis of the directions of the principal in-situ stresses. The directions were in agreement with those determined for the same region using stress relief method. In addition, the predicted principal stress values ranged between those of the major and minor principal stresses which were independently determined by differential strain curve analysis using cores extracted from nearly the same depth in the same well. The results obtained show that the ASR method is well suited to be used to determine in-situ stresses at great depth.
机译:以六个独立的方向测量从深阱中的4500m MD的深度取出的导向核心的Anelast菌株恢复(ASR)。回收的凹凸式菌株用于三维分析本原位应力的方向。使用应力浮雕方法对同一区域确定的那些方向一致。另外,预测的主应力值之间的主要和次要主应力的范围,其通过差分应变曲线分析使用从相同的孔中的几乎相同深度提取的芯而独立地确定。得到的结果表明,ASR方法非常适合于用于在极深的原位应力。

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