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Inflation and deflation of deeply buried salt stocks during lateral shortening

机译:侧向缩短过程中深埋盐层的通货膨胀和放气

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We used scaled physical models to investigate how buried, dormant diapirs are rejuvenated by lateral squeezing. In Stage 1, regional shortening increased the pressure of the source layer, causing an inward plume of source-layer salt to intrude the dilating diapir and arch its roof. In Stage 2, the thrust front jumped forward to the salt stock, forming a major salient toward the foreland, and the stock roof was arched. Salt inflation still dominated, but a small outward plume of diapiric salt began to intrude the source layer on the foreland side of the diapir. With continued shortening in Stage 3, the converging diapir walls deflated the diapir, while a major overthrust prevented surface extrusion. Compressional uplift of the overburden created space for downward intrusion of diapiric salt into the source layer and diapiric pedestal. The models document a newly recognized type of active diapir that inflates under compression. The models also show how a salt diapir can weld shut where surface extrusion of salt is inhibited.
机译:我们使用了比例缩放的物理模型来研究侧向挤压如何使埋藏的休眠底盘恢复活力。在阶段1中,区域缩短会增加源层的压力,从而导致源层盐的向内羽流侵入扩张的diapir并使其顶棚拱起。在第2阶段中,逆冲前缘跃升至盐储层,形成朝向前陆的主要突出部分,并且储藏室顶部呈拱形。盐的膨胀仍然占主导地位,但是一小片向外扩散的二apiapi盐开始侵入底辟的前陆侧的源层。随着第3阶段的持续缩短,会聚的水坝壁使水坝缩小,而较大的上推力阻止了表面挤压。上覆岩层的压力抬升创造了空间,使二apiapi盐向下侵入源层和二api基座。这些模型记录了一种新认识到的活动型Diapir类型,它在压缩状态下会膨胀。该模型还显示了盐底皮堆如何在盐的表面挤压受到抑制的地方焊接关闭。

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