• 成矿机理韧性剪切变形动力成岩成矿。

    The mineralization mechanism is that the brittle-ductile shearing deformation dynamically resulted in diagenesis and mineralization.

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  • 其特点整体有序无序韧性剪切变形强烈

    The rock group is characterized by a general order but internal disorder because of intense ductile shearing deformation.

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  • 成矿主要与脆性变形有关,韧性剪切变形脆性剪切变形转变至关重要

    It is very important for the change from ductile to brittle shear strains.

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  • 印支末期—燕山遭受了吴川四会断裂带的左行走滑韧性剪切变形变质作用

    In last Indonian-Yenshan Stage, They also underwent left-slipping ductile Shear deformation and metamorphism along Wuchuan-Sihui fault belt.

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  • 晚期韧性剪切变形与区域D_3变形幕有关,伴随绿泥石、冻蓝闪石出现石英方解石动态重结晶作用

    The late ductile shearing(DF_2) formed in D_3 deformation phase is accompanied by the appearance of chlorite and barroisite etc. and dynamic recrystallization of albite, quartz and calcite.

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  • 燕山期,该构造带脆性-脆性断裂变形为主,在早期韧性剪切变形的基础叠加一系列同方向的角度压性-压扭性断裂

    In Ysashanian stage, it was characterized by ductile brittle and brittle faulting and formed a series of east west trending high Angle thrust faults superposed on the early mylonite zones.

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  • 大多数情况下韧性剪切中的变形岩石为糜棱岩,因为经受韧性剪切变形时,岩石粒度显著减小发育了强化的叶理(线)。

    In most cases, the deformed rocks within ductile shear zones are mylonites, because rock grain size obviously reduced and strengthening foliation (lineation) developed.

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  • 韧性剪切变质变形作用但是变质变形作用过程而且也是重要成矿作用过程

    The ductile shear process is not only metamorphism and deformation but also an important mineralization process.

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  • 兴隆金矿区韧性剪切兴隆沟断裂影响,韧性剪切变质变形控制着本区金矿(化)空间分布

    Influenced by deep fracture, the ductile shear metamorphism and deformation of Xinglonggou ductile shear belt control the space distribution of gold ore body in this mining area.

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  • 位于雪峰弧形构造中段江东湾金锑矿床,其空间定位矿体展布阳-溆浦韧性剪切控制,矿区内岩石剪切变形特征明显。

    The Jiangdongwan gold-antimony deposit is located in the middle part of Xuefeng arc structural belt and controlled by the Qianyang-Xupu ductile shear zone.

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  • 位于雪峰弧形构造中段江东湾金锑矿床,其空间定位矿体展布阳-溆浦韧性剪切控制,矿区内岩石剪切变形特征明显。

    The Jiangdongwan gold-antimony deposit is located in the middle part of Xuefeng arc structural belt and controlled by the Qianyang-Xupu ductile shear zone.

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