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.
三组室内模型试验表明具有软弱下卧层的地基破坏模型基本上属于冲切破坏。
Three sets of model test in laboratory show that the failure model in the foundation with soft clay underlying layer belongs basically to the punching shear failure.
褶皱-冲断带和盐相关构造均十分发育的秋立塔克地区构造极其复杂，该地区新生界内部存在两套起滑脱层作用的膏盐层。
Fold-thrust belts and salt-related structures are very prevalent in the Kuqa foreland fold-thrust belt of Tarim Basin in Northwest China.
下第三系的构造变形主要表现为区内下第三系红层的逆冲断块和宽缓褶皱变形。
The structural deformation of the Paleogene is characterized evidently by thrust block and broad folds.
松树沟逆冲推覆构造研究对恢复蛇绿岩组合层序及其古构造环境具有重要的地质意义。
Studing the thrust-nappe help us to re-establish the Songshugou ophiolite sequence and its ancient tectonic environment.
本机适用于皮革、塑料、尼龙布、纸板、泡棉及合成纤维、非金属材料的成型裁断作业，特别适用于宽幅材料的一层或多层冲裁落料。
Its suitable to scissor up leather plastic, nylon, paper, carton sponge and synthetic fibres, in particular it is suitable to cut single layer or multilayer broad width materials.
本机适用于皮革、塑料、尼龙布、纸板结、泡棉及合成纤维、非金属材料的成型裁断作业，特别适用于宽幅材料的一层或多层冲裁落料。
It is suitable to scissor up leather plastic nylon paper carton sponge and synthetic fibres, in particular it is suitable to cut single layer ot multilayer broad width materials.
厄尔士山脉变质沉积物的地球化学识别和对比表明在变质逆冲单元中重现了早古生代变质沉积层序。
Geochemical discrimination and correlation from the metasediments of the Erzgebirge suggest repetition of an early Palaeozoic metasedimentary sequence in metamorphic thrust units.
采用实验的方法，系统测定了苔藓层在抗冲性、抗雨蚀性以及持水能力等方面的效益。
Using the method of experiment, the benefits of Bryophyta layers on anti-scourabili-ty, rainfall erosion-resistant and water-holding capacity are comprehensively determined.
逆冲带近端、远端与盆地中部沉积物源供给不同，决定了盆地内不同部位的层序发育样式和准层序的叠置形式不同。
The difference of depositional supply of near thrust belt and far thrust belt made the depositional filling and stacking patterns of parasequences different.
在排水沟、雨水口处找出泛水，冲筋后即可进行抹找平层。
It finds flashing at draining ditch and rain water opining. It can begin leveling with trowel after screeding.
在逆冲断裂的下盘，是一套正常沉积层序的地层，分别为侏罗系、三叠系、石炭—二叠系、寒武—奥陶系等地层。
There is a normal deposition sequence stratigraphy beneath the lower wall of over-thrust fault, such as Jurassic, Triassic, Permian-Carboniferous, Cambrian-Ordovician system.
在逆冲断裂的下盘，是一套正常沉积层序的地层，分别为侏罗系、三叠系、石炭—二叠系、寒武—奥陶系等地层。
There is a normal deposition sequence stratigraphy beneath the lower wall of over-thrust fault, such as Jurassic, Triassic, Permian-Carboniferous, Cambrian-Ordovician system.
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