• 然后这些沉积物可能形成褶皱和叠瓦构造。

    This sediment will then probably be formed into a folded and imbricated structure.

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  • 南秦岭自北向南产生低角度叠瓦状逆冲断裂。

    The south Qinling has formed an imbricated thrust fault at low angle from the north to the south.

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  • 把你的容身之处的屋顶看作是一间房子的叠瓦状。

    Think of your shelter roof as being shingled like a house.

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  • 其构造类型主要为断层相关褶皱、叠瓦状构造及断层三角带。

    The structural types mainly are fault-related folds, imbricate structure and fault delta zone.

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  • 北秦岭为一复杂构造带,形成向北反转的叠瓦状逆冲推覆构造。

    The north Qinling is a complicated structural zone, forming an imbricated thrust napped structure overturning northward.

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  • 在剖面上,叠瓦冲断带位于三角带构造的前缘下方,平面上呈重叠分布。

    On the section, the imbricate thrust zone is situated below the front margin of the triangular-zone structure, and they are overlapping distributed on plane.

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  • 该推覆体由数条撕裂断层分为几个叠瓦体,各有不同的形态、结构特征。

    This nappe group is divided into several imbricates by several tear faults, each of which has different features with respect to its shape and structure.

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  • 野外判定岩浆岩地区逆冲推覆构造的主要标志是逆冲叠瓦扇和软弱滑动层的存在。

    The imbricate fan of thrusts and soft layer are main structure features distinguishing thrust-nappe structure in magma-tic body area.

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  • 根据与其它气田构造的对比,穿盐断裂和叠瓦冲断带的构造组合样式对油气的聚集最为有利。

    The most efficient structural assemblage zone for gas accumulation is the thrust fault and nappe thrust belt developed in a variety of salt-related due to tectonic compression and salt flexible fluid.

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  • 中期(喜马拉雅早期)是主变形期,西带显示由SW向NE逆冲,以叠瓦状逆冲构造系统为其特征。

    The middle(early Himalayan)is the main deformation, characterized by the imbricate thrust structure system, whose west zone shows thrusting from SW toward NE.

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  • 推覆构造体系是由几条逆冲断裂带及其逆冲席、逆冲片组成,主干断层与次级断层组成叠瓦式构造。

    The structural system of nappe consists of several overthrust fracture belts, thrust sheets and thrust slices, and master fault and secondary fault form an imbricate structure.

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  • 由北向南分为前缘挤压滑脱构造带、斜歪倒转褶皱—逆冲断层带和逆冲推覆岩席及叠瓦状逆冲断层带。

    From north to south, several tectonic belts can be distinguished: front compressive detachment belt, overturned thrusting belt, sheeted thrusting belt and imbricate thrusting belt.

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  • 该项目的设计重新诠释了传统的互搭壁板,定制的、叠瓦状的反光玻璃幕墙像鱼鳞一样覆盖整座建筑。

    The design reinterprets traditional lap siding with a custom, shingled glass facade of reflective panels that are overlaid like fish scales both vertically and horizontally across the entire building.

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  • 针对叠瓦式构造底板的特殊结构形式,在分析受力情况的基础上,提出了应用于该结构形式底板的抗滑稳定计算公式;

    Based on analysed of pressure which act on imbricate structure soleplate, we educed the static force anti-sliding stability formula;

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  • 盆地中发育多种构造样式,主要有:叠瓦状冲断层、滚板构造、牵引褶皱、铲形正断层、滚动背斜、“垒一堑”构造等。

    The structural style found in the basin includes imbricated thrust zone, trapdoor structure, drag fold, listric fault, rollover anticline, horst-graben structure and the like.

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  • 这些特点说明,该盆地具有伸展成因的裂谷性质,盆地的形成可能与沿着有根的叠瓦式低角度剪切断裂系发育的地壳伸展作用有关。

    The formation of the basin might be probably related to crustal extension controlled by a series of imbricate, low-angle, rooted shear faults.

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  • 队友是否在进攻中可以主动上前援助你,以牺牲稳固防守为价钱制造叠瓦式助攻跑动,这对角逐战术来说会表现出截然不同的效验。

    It makes a huge difference to how players will support you in attack, making overlapping runs at the expense of defensive discipline. Here's the full list…

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  • 研究区构造应力场主要为挤压应力场,区内主要形成褶皱、断弯褶皱、断展褶皱、叠瓦逆冲构造、冲起构造和逆冲三角构造等构造样式。

    The stress fields are compression ones, in that conditions, the structure styles are folds, Fault-bend folds, Fault-Propagation folds, Detachment folds, imbrications-thrust faults and so on.

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  • 提出二叠纪时期冈底斯带可能为一个在古特提斯洋盆中呈条块状“漂浮”的冈瓦纳碎片。

    They propose that during the Permian the Gangdise belt might be a fragment of Gondwana that floated in the Paleo-Tethyan Ocean.

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  • 由此本文认为麻扎-康西瓦-苏巴什结合带经历了震旦-早志留世的原特提斯洋的演化和中泥盆世-早三叠世的古特提斯洋的演化;

    Therefore, this paper thought that Mazha-Kangxiwa-Subashi suture zone experienced Sinian to Early Silurian evolvement of Proto-Tethys and Devonian to Early Triassic evolution of the Palaeo-Tethys ;

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  • 由此本文认为麻扎-康西瓦-苏巴什结合带经历了震旦-早志留世的原特提斯洋的演化和中泥盆世-早三叠世的古特提斯洋的演化;

    Therefore, this paper thought that Mazha-Kangxiwa-Subashi suture zone experienced Sinian to Early Silurian evolvement of Proto-Tethys and Devonian to Early Triassic evolution of the Palaeo-Tethys ;

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