薄皮构造

安徽下扬子区北缘薄皮构造之表层构造丰富、典型；

The thin-skinned tectonics in the northern fringe of Anhui Lower Yangtse region has typical surficial structures .

鄂皖边界大别南缘主俯冲边界断层的存在以及扬子板块前陆盆地盖层大型薄皮构造，揭示扬子板块向大别造山带之下的A型俯冲。

The main A-type subduction fault and large scale thin-skinned tectonics clearly reveal that the Yangtze Plate subsides towards Dabie orogenic belt .

逆冲构造具有基底卷入的厚皮构造与盖层内部的薄皮构造共存的构造属性，上盘运动方向总体指向NW，逆冲构造变形主要发生在140~130Ma。

Thrust tectonics in this area are characterized by the combination of basement-involved thick-skinned structures and only cover sequence-involved thin-skinned structures , with top-to-the-northwest thrusting during 140 ~ 130Ma .

川东薄皮构造模式之我见

My opinion of structural pattern of thin-skinned structure in East Sichuan

薄皮构造的突发隆起带及韧性滑脱面分别是寻找油气和金的有利地带。

The pop-up is the advantageous oil and gas belt , and the ductile detachment is that of Au .

喀拉玉尔滚右旋走滑断层为薄皮构造，调节了却勒地区东、西段前缘的变形差异。

Karayulgun dextral strike-slip fault , which is a thin-skinned structure , adjusted the deformation difference located at frontal range of Quele area .

在外营力的剥蚀与破坏影响下，薄皮构造受到程度不同的剥蚀破坏而呈现出不同的褶曲形态。

By the action of exogenetic force , the thin-skinned structure was subjected to denudation to varying degree , appearing as different folded forms .

薄皮构造以单剪方式往南东运动，缩短量达94km，缩短率约63.4%；

The wedge moves towards southeast in simple shear way , and the shortening amount is about 94 km while the shortening rate is 63.4 % .

华北陆块北缘西段狼山-渣尔泰山裂陷槽西延的地质依据及其意义华北地块南缘向北的薄皮推覆构造及北秦岭加里东造山作用

Northward thin-skinned nappe structure in the southern margin of North China landmass and Caledonian orogeny in northern Qinling

尺度物理实验用干石英砂和聚合硅树脂为实验材料，模拟了前陆褶皱冲断带厚皮缩短盐构造，并与薄皮缩短盐构造及无盐层的褶皱冲断带构造模型进行了对比。

Scaled physical modeling investigated structures formed during thick-skinned contractional salt tectonics in a foreland fold-and-thrust belt . Dry quartz sand simulated brittle sedimentary rocks , and viscous silicon polymer simulated viscous rock salt .

通过对华北地块南缘向北的薄皮推覆构造及北秦岭构造带结构、构造特征分析，认为它们同属于加里东期造山作用产物。

Analysis of the northward thin-skinned nappe structure in the southern margin of North China landmass and the textures of the structural belt in northern Qinling suggests that they all belong to the results from Caledonian orogeny .

京西煤田马兰薄皮式推覆构造

The thin skin type nappe structures in malan , western Beijing coal field

伴随挤压变形，在造山带及其前渊产生由厚皮到薄皮的复杂变形构造。

Complex structural deformation , from thick skinned to thin skinned structures , has occurred in the orogenic belt and its frontal region along with compressional deformation ;