首页> 外文会议>Third International Symposium on Rock Stress (RS KUMAMOTO '03); Nov 4-6, 2003; Kumamoto, Japan >Determination of rock stress by anelastic strain recovery measurement of an oriented core in the Nittsu region of Japan
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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:通过日本Nittsu地区定向岩心的无弹性应变恢复测量确定岩石应力

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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:从六个独立方向测量了深井中深度为4500 m MD的定向安山岩芯的无弹性应变恢复(ASR)。回收的无弹性应变用于原位应力方向的三维分析。方向与使用应力消除方法为相同区域确定的方向一致。此外,预测的主应力值介于主,次主应力之间,该主应力是通过使用从同一井中几乎相同深度提取的岩心通过差分应变曲线分析独立确定的。获得的结果表明,ASR方法非常适合用于确定较大深度的原位应力。

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