• 新元古界双桥山上亚千枚、 板

    Upper Neoproterozoic Shuangqiaoshan Group phyllite, arenopelitic shale;

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  • 新鲜绢云母石英千枚岩新鲜变粒

    The rock mass consists of fresh sericite quartz phyllite or fresh leptynite.

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  • 通过现场的室内三轴试验研究炭质千枚岩蠕变特性。

    A laboratory triaxial creep test to on-site specimens is carried out to study the creep properties of the carbonaceous phyllite.

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  • 大别山北部佛子岭变碎屑主要由板枚岩云母石英所组成。

    Foziling Group in the Dabie Mountains is composed of SLATE, phyllite, mica quartz schist, etc.

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  • 该类矿床产于古元古代富硼、碳千枚岩夹石英)建造之中;

    This type deposit is formed in the formation of B-rich and C-rich phyllite with quartzite (siliceous rocks) as intercalated beds, which belongs to early Proterozoic Laoling group;

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  • 西汉出露于盆地南部千枚岩为主夹灰生物礁;

    The Xihanshui Group, which distributes in the southern of the basin, is mainly slates, phyllites and sandstones with carbonatite and reef blocks.

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  • 乌鞘岭隧道脊段志留系地层千枚夹板地段,施工中发生变形,初期支护开裂破坏甚至

    Severe deformation occurred at the siluric stratum at the ridge of Wushaoling Tunnel, causing splitting of primary lining and even exceeding clearance limit.

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  • 类型主要有云母石英石英大理千枚岩等,因富含炭质而呈灰色,灰黑色。

    The rocks of this Formation, which are black or light black for rich of c, consist mainly of mica quartz schist, quartzite, marble, carbonaceous phyllite.

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  • 主要有变泥质粉长石石英细砂质长石石英粉砂、长石杂砂云石英千枚岩

    Its main rocks is the metamorphic pelitic siltstone, the feldspathic quartz wacke, the fine sandial feldspathic quartz siltstone, the feldspathic wacke and the sericite quartz phyllite etc.

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  • 页水铅锌矿床位西秦岭西成矿西南部,容矿泥盆统广金坝组第三段中的灰枚岩等。

    The Yeshuihe lead-zinc deposits are located in the southwest part of the Xicheng orefield in the west Qinling. The host rocks are the third member of the middle Debonian Guangjingbar Formation.

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  • 页水铅锌矿床位西秦岭西成矿西南部,容矿围泥盆统广金坝组第三段中的千枚岩等。

    The Yeshuihe lead-zinc deposits are located in the southwest part of the Xicheng orefield in the west Qinling.

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  • 地壳主要为绿(部分低角闪相)千枚岩、变粒以及花岗组成,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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  • 地壳主要为绿(部分低角闪相)千枚岩、变粒以及花岗组成,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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