• 断裂带存在岩石绿泥石新形成的逆行绿片岩叠加

    The pre-exist amphibolite facies rocks in the fracture belt have been superimposed by retrograde green-schist facies with neoformation of chlorite.

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  • 绿片岩以下动力变质作用矿化富集条件

    Dynamical metamorphism under greenschist facies is the condition of mineralizing enrichment.

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  • 川西高原广泛分布的西康,原视为区域低温动力变质作用绿片岩变质

    Xikang Group is widely exposed on the West Sichuan Plateau and was considered to be a low greenschist facies metamorphic rock due to regional low-temperature dynamometamorphism.

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  • 变质基底角闪岩绿片岩逐渐过渡为上覆盖层的低绿片岩相

    The metamorphic facies gradually change from low amphibolitehigh green-schist facies of the basement to low green-schist of the cover.

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  • 变形强烈塑性变形变形,变质角闪岩到低绿片岩及低于低绿片岩相

    The deformation was changing from plastic intensity to weakness and the metamorphic facies ranged from amphibolite to low-grade greenschist.

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  • 早期韧性变形发生在角变质作用条件晚期的脆韧性变形发生在绿片岩变质作用条件下。

    The earlier ductile deformation took place under the condition of amphibolite facies and the later transitional ductile-brittle deformation under the condition of greenschist facies.

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  • 地壳主要为绿片岩(部分低角闪)板岩、千枚岩、片岩、变粒以及花岗岩组成,顶部沉积盖层。

    The upper crust is mainly composed of slates, phyllites, schists, granulite of greenschist facies (partly low-amphibolite facies) and granite intrusions, and sedimentary rocks at the top.

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  • 放牛石英岩系为经绿片岩变质的陆源碎屑岩。、底界线清晰下伏太古宙变质花岗岩系上覆中元古界熊耳均呈角度不整合接触。

    Fangniushan quartzite series consist of coarse terrigenous clastic rock which has been suffered the metamorphism of low green schist facies, contact lines of its top and base are distinct.

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  • 喜马拉雅构造迦巴瓦岩群石榴辉石岩透镜产于麻粒变质的长英质片麻岩泥质片岩之中。

    Garnet pyroxenite occurs as lenses in granulite-facies metamorphic granitic gneiss and pelitic schist in the Namjagbarwa Group-complex of the eastern Himalayan tectonic syntaxis.

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  • 根据浆-矿物平衡热力学,岩浆认为起源于辉岩条件下俯冲板片的部分熔融。

    Based on the melt-mineral equilibrium thermodynamics, it is believed that the adakitic magma originated by partial .

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  • 泰山地区阜平期麻岩英云闪长质片麻岩、奥长花岗质片麻岩组成,呈西向带状分布形成于角环境,岩石普遍具片麻状构造,局部地区岩石的韧性作用比较强烈。

    The Fuping-time gneiss in the Taishan area, consisting of tonalite gneiss and trondhjemite, formed in NW zonal distribution in the amphibolite -facies temperature and pressure environment.

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  • 泰山地区阜平期麻岩英云闪长质片麻岩、奥长花岗质片麻岩组成,呈西向带状分布形成于角环境,岩石普遍具片麻状构造,局部地区岩石的韧性作用比较强烈。

    The Fuping-time gneiss in the Taishan area, consisting of tonalite gneiss and trondhjemite, formed in NW zonal distribution in the amphibolite -facies temperature and pressure environment.

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