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Duplex and along-strike structural variation: A case study from Sikkim Himalayan fold thrust belt

机译:双重构造和沿走向构造变化:以锡金喜马拉雅褶皱逆冲带为例

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摘要

The Sikkim Lesser Himalayan fold thrust belt records along-strike structural variations over 15 km. The lower Lesser Himalayan (Rangit) duplex (LHD) is blind, and the overlying Pelling and Ramgarh thrust sheets are more intensely folded and preserved in eastern Sikkim than in western Sikkim. A retrodeformable, regional balanced cross-section reveals a minimum shortening of similar to 403 km (similar to 80%) with an average long-term shortening rate of similar to 18 mm/yr in the eastern transect. Comparison with published data indicates that eastern Sikkim records similar to 47 km lesser shortening. In western Sikkim, an similar to 2km high footwall Main Himalayan thrust (MHT) ramp below the Rangit duplex caused higher structural culmination exposing the duplex. In contrast, an similar to 0.35 km high ramp below the Rangit duplex in eastern Sikkim did not create sufficient culmination to expose the duplex, causing along-strike discontinuous duplex exposure. The LHD with a blind component, and having fewer (11) but gentler dipping (40) horses transferred more displacement to the roof thrust in eastern Sikkim than the twelve, steeper dipping (60) horses in western Sikkim. Lateral variations in location and height of footwall MHT ramp, initial width of the Lesser Himalayan basin, and presence of a lateral ramp explain the structural variation in Sikkim.
机译:锡金小喜马拉雅褶皱逆冲冲断带记录了15 km沿走向的构造变化。小喜马拉雅山脉(Rangit)较低的双眼(LHD)失明,锡金东部的褶皱和拉姆加推力板折叠和保存程度比锡金西部要强。可逆变形的区域平衡横截面显示,东部断面的最小缩短量约为403 km(约80%),平均长期缩短率约为18 mm / yr。与已公布数据的比较表明,锡金东部记录的缩短时间缩短了47公里。在锡金(Sikkim)西部,一个接近2公里高的下盘墙在朗吉特双峰下方的喜马拉雅山主推力(MHT)坡道引起了更高的结构顶点,从而暴露了双峰。相反,在锡金东部的朗吉特(Rangit)复式岩层以下,类似于0.35 km的高坡道并没有产生足够的高潮来使复式岩层暴露,导致沿走向的不连续复式岩层暴露。与锡金西部的十二只陡峭的马匹(60只)相比,具有盲目分量的LHD少(11匹)但较缓的马匹(40匹)使锡金东部的顶推力转移到位移更大的位置。底墙MHT坡道的位置和高度,小喜马拉雅盆地的初始宽度以及存在一个横向坡道的横向变化解释了锡金的结构变化。

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