• The intermediate-acid pyro-clastic rock is dominant with a few of intermediate lava and common sedimentary pyroclastic rocks formed in the volcanic intermittent activities in the Qidaogou area.

    秋皮沟一带分布酸性火山碎屑为主,夹少量中性熔岩火山间歇期正常沉积秋皮沟火山碎屑

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  • Therefore, the protoliths of the UHPM rocks from the southern Sulu orogenic belt were sedimentary rocks, mafic and acidic volcanic rock, granite and trondhjemite formation with continental affinity.

    因此,可以推测苏鲁山带核部超高压变质原岩为形成在大陆板内环境的沉积岩-酸性基性火山岩-花岗岩和奥长花岗岩建造。

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  • Their original rocks are volcanic rocks, epicontinental clastic sedimentary rocks, and ophiolite of volcanic and island arc tholeiitic series or calcium alkali series.

    岩岩石类型火山岩陆缘碎屑沉积岩火山岛弧拉斑系列系列火山岩、绿岩等。

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  • The primary rocks include the various sodium-rich volcanic rocks and the sedimentary rocks with sodium-rich volcanic materials which are well developed in the North Qilian eugeosyncline area.

    区内含蓝闪石岩包括优地槽内发育各类火山岩、含富钠火山质的沉积岩

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  • The Hongtaiping polymetallic deposit lies in the Permian Marine volcanic rocks, Palaeozoic geosyncline and the transitional belt of the clastic sedimentary rocks in the Yanbian area.

    太平多金属矿床产于延边古生代地槽区叠系海相火山岩及其与碎屑沉积岩过渡带上。

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  • Changling fault depression is a basin of continental volcanic-sedimentary rocks, faulting is the key factor that controls volcanic activities and volcanic rock distribution.

    长岭陆相火山岩沉积岩盆地断裂运动控制火山活动火山岩平面分布主要因素

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  • The gold mineralization is controlled by lower carboniferous volcanic and pyroclastic sedimentary rocks, regional faults and secondary structure.

    论述下石炭火山岩火山碎屑沉积岩区域性大断裂及次级构造对成矿控制作用。

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  • The sedimentary facies developed mainly include alluvial fan, fluvial, lake flat, lacustrine, fan delta, delta, lake-floor fan and volcanic rocks.

    发育沉积相类型有冲积相、河流相、湖漫、湖泊相、扇三角洲相、三角洲相、湖底扇相和火山岩相。

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  • The Tongbomiao Formation consists of pyroclastic, volcanic-sedimentary and terrigenous clastic rocks in Beier sag, Hailaer Basin.

    海拉尔盆地贝尔凹陷庙组发育一套火山碎屑岩类、火山-沉积岩类少量陆源碎屑岩石组合。

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  • The volcanic rocks associated with the terrigenous elastic rocks and intrabasinal sedimentary rocks predominate in the Devonian strata in the Ashele and Chonghur regions, Xinjiang.

    新疆阿舍勒乎尔地区泥盆纪地层火山岩为主,伴有陆源碎屑内源沉积岩

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  • The upper part of it is a suit of metamorphic flysch formation, and the lower part, metamorphic volcanic-sedimentary rocks.

    上部变质复理石建造下部为变质火山-沉积岩建造。

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  • The upper part of it is a suit of metamorphic flysch formation, and the lower part, metamorphic volcanic-sedimentary rocks.

    上部变质复理石建造下部为变质火山-沉积岩建造。

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