首页> 外文期刊>Proceedings of the Yorkshire Geological Society >Syn-sedimentary deformation of the Ashover Grit(Pennsylvanian,Namurian, Marsdenian Substage)deltaic succession around Wirksworth, Derbyshire, UK
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Syn-sedimentary deformation of the Ashover Grit(Pennsylvanian,Namurian, Marsdenian Substage)deltaic succession around Wirksworth, Derbyshire, UK

机译:英国德比郡Wirksworth周围的Ashover砂砾(Pennsylvanian,Namurian,Marsdenian Substage)三角洲次生沉积变形

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摘要

Three sets of syn-sedimentary slides affecting delta deposits of the Ashover Grit have been identified in the area south and east of Wirksworth, Derbyshire, UK. The kilometre-scale slide masses, which are expressed clearly in the landscape, consist of arrays of fault blocks tilted back towards listric fault surfaces that sole out into underlying basinal mudstone. Relationships in one of the slide arrays, at Black Rock, suggest that the movements took place during the later stages of delta advance. There is a possibility that some minor compressional structures exposed in surface sections away from the fault blocks are also related to syndepositional movements.
机译:在英国德比郡Wirksworth的南部和东部地区,发现了三套影响Ashover砂砾三角洲沉积的同沉积滑坡。在地形中清楚表达的千米规模滑坡体由断层块阵列组成,这些断块块向着倾斜的断层表面倾斜,这些断层表面向底层的盆地泥岩中突出。在黑岩(Black Rock)的一个幻灯片阵列中的关系表明,运动发生在三角洲晚期的后期。在远离断层块的表面区域暴露的一些较小的压缩结构也可能与沉积运动有关。

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