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We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

在综述前人认识的基础上,笔者通过对中国前陆盆地的构造演化历程、沉积充填特征、构造成因及其空间分布规律、构造变形特征等的研究,提出了中国前陆盆地构造地质发育的5个主要特征:(1)两种不同性质的原型盆地发生正反转的叠合性,即挤压构造下作为&本体&的前陆层序与拉张构造下作为&基础&的裂谷、断陷盆地之间的叠置;(2)显生宙以来中国大陆先后发生了4期前陆冲断构造演化的多期性,它们分别是加里东晚期、海西晚期、印支期和喜马拉雅晚期;(3)基于小克拉通基底拼贴后在造山带前缘复活再生的继承性,即统一拼合大陆内部的构造变形导致古造山带的复活,在古造山带边缘发育新生代前陆盆地或前陆冲断带;(4)在空间分布上受环青藏高原巨型盆山体系控制发生陆内变形的系统性,在环青藏高原巨型盆山体系内构造变形强度、盆地沉降幅度、盆山耦合程度等从内环向外环依次降低,从古造山带向克拉通方向构造变形强度依次降低,构造变形样式逐渐简单、构造变形时间依次变新;(5)前陆冲断带的构造样式由于受边界力学条件和沉积地层介质作用而具有多变性,存在沉积盖层内脆性变形的断层相关褶皱、造山带前缘韧性变形的基底卷入构造、与走滑构造相伴生的基底卷入的断层相关褶皱、盆地内部塑性变形的盐构造。

Squeeze pressure, generated by contraction of the external anal sphincter and puborectalis muscle, more than doubles intra–anal canal resting pressure.

挤压力主要由外括约肌及耻骨直肠肌的收缩产生,通常是静息压的2倍。

The three tectonic movement formed the pulsant compression orogenic character of late Caledonian.

这三次构造活动构成了加里东晚期脉动性挤压造山特点。

The results show that dendrites in casting are converted into directional micro-crystals, and then recrystallize and grow into spheroidizing grains.

结果表明:铸造状态下的树枝状组织在挤压预热过程中形成了带有方向性的小结晶,之后再成长为显微结晶,观察到了变化为球状的结晶粒。

He TiC could reprecipitate again with excess milling and Cu crystal decreasing. TiC-dispersion-strengthened Cu-based composite powders have been prepared from TiC-Cu and Cu-Ti-C mixed powders by MA. The composite powders were prepared into composite materials by pressing, sintering and heat-extrusion.

IC混合粉末经机械球磨后,再经压制、烧结和热挤压制备成 n 弥散强化铜基复合材料。

The rheological properties of soy protein dough were investigated using a capillary rheometry and a viscosity model based on the experimental results was also presented.

食品物料在挤压过程中流变行为的研究是一个研究热点。对于大豆蛋白质面团流变性能测试和黏度模型的研究,国外学者做了不少工作。

Type I is composed of rhyolitic rocks, which are characterized by higher Si and alkali contents and lower Al and Ti contents, Na2O/K2O1 and a weak negative Eu anomaly (δEu=0.65–0.95), enriched in Sr and Ba and poor in Rb. Types I and II probably formed in an extensional to postorogenic extensional environment, accompanied by compressional uplift.

提要:大兴安岭北段根河地区早白垩世火山杂岩按岩石及其地球化学特征,可划分为3类:第Ⅰ类为流纹质岩石,富Si,碱,低Al,Ti,Na2O/K2O1,具弱的负Eu异常(δEu=0.65~0.95),富Sr,Ba,贫Rb;研究认为第Ⅰ,Ⅱ类岩石产于挤压隆升相伴的拉张至造山后伸展构造环境。

You ruffed a heart with the spade queen, and West was backwash-squeezed.

你现在用Q将吃红心,而西被回流挤压

Sapa is an experienced extrusions operator and has a better chance of improving profitability before a possible IPO of the business.

Sapa是一家经验丰富的挤压厂运营商,在实现上市前我们仍有机会改善工厂的业绩。

Objective:To study the effects of nerve growth factor on regeneration of crushed sciatic nerve in rats.

目的:观察肌注神经生长因子对大鼠坐骨神经挤压伤后的促再生作用。

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