递进变形

拉张状态下方解石组构的递进变形规律

The regulation of progressive deformation on calcite fabric in stretch state

蛇绿混杂岩破碎混合作用记录了一种递进变形的应变历史。

The disrupting and mingling of the melange may record a strain history of progressive deformation .

它们是在北西南东向挤压作用下递进变形的结果。

They are a result of the progressive deformation in NW SE compression .

它们的形成与岩石变形变质作用有密切关系，形成和演化过程可分为3个阶段：递进变形变质阶段；

The processes of their formations and evolutions can be devided into three phases : progressive deformation and metamorphism phase ;

并对加速蠕变和应变软化两种情况，给出了不同时刻韧性剪切带内的温度、应力、应变、应变率、位移和粘滞系数的分布特征，描述了岩石递进变形的规律。

The distributions of temperature , stress , strain , strain rate , displacement and viscous damping coefficient within ductile shear zone at different time intervals are distinguished in the cases of accelerating creep age and strain softening .

成矿以发育含矿热液的脆韧性递进剪切变形构造控制为关键，直接控制了工业矿体的分布、矿化强度与就位。

The hydrothermal fluid-bearing brittle-ductile shear zone , which is progressively deformed is the key structure to control mineralization degree and industrial ore bodies emplacement directly .

它是江南&雪峰基底拆离推覆体由SE向NW方向水平挤压作用下中上扬子古生界盆地沉积盖层产生递进（衰减）变形的结果。

When the Jiangnan-Xuefeng basement decoupling nappe horizontally extruded from SE to NW , the sedimentary cover of Middle-Upper Palaeozoic basin progressively ( decreasingly ) deformed and resulted in kink structure .

它使扬子海相中古生界盆地发生了由强及弱的递进（衰减）变形改造。

It causes to make the Middle Palaeozoic marine sedimentary basins going forward one by one through powerful and feeble ( Attenuation ) deformation is reformed .

晚期的右旋高角度斜冲非共轴递进剪切使弱变形域中央最发育的一组节理和裂隙由压性转变为张性，并沟通深部的裂隙系统。

In the late period , the progressive uncoaxial shear of right-lateral and high-angle oblique thrusting caused the most developed joints and fractures in the core of weak-deformation domain to turn from compressional to extensional , and linked up with deep fracture systems .