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“郯-庐断裂带南段深层次的塑性变形特征及区域应变场”(以下简称“郯-庐带应变场”)一文(发表于本刊,1984,第6卷,第4期)作者认为,郯-庐断裂带南段是一个对应于郯-庐断裂带深层次的大型平移韧性剪切带,并根据变形砾石讨论了区域应变场,用剪切的片理面、劈理面走向、褶皱轴迹以及原始片理面上的拉伸线理(经过展平)作为拉伸构造线的标志测量θ′角并计算位移量。同时还讨论了应变在垂深(实为地层)
“The deep plastic deformation features and the regional strain field in the southern section of the Xun-Lu fault zone” (article published in 1984, Volume 6, Issue 4) . The southern section of the Xuan-Lu fault zone is a large-scale transgressive ductile shear zone corresponding to deep deep strata of the Tie-Lu fault zone. Based on the deformed gravel, the regional strain field is discussed. The shear facets, cleavage planes, The wrinkle axis and the stretching principle (flattened) on the original facet are measured as the θ ’angle of the tensile construction line and the displacement is calculated. At the same time also discussed the strain in the vertical depth (in fact, the formation)