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Physical Models of Thick-Skinned Contractional Salt Tectonics in a Foreland Fold-and-Thrust Belt

前陆褶皱冲断带厚皮缩短盐构造运动的物理模拟

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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.

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。

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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.

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。

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