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A new 'microstructural mapping' methodology for the identification, analysis and interpretation of polyphase deformation within subglacial sediments

机译:一种新的“微观结构图”方法,用于识别,分析和解释冰下沉积物内的多相变形

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摘要

Although integrated clast macro and microfabric studies have been used to provide evidence of palaeo-ice flow directions, to discriminate between diamictons deposited in differing sedimentary environments, and to model the response of tills to subglacial deformation, such studies have typically only examined the ‘bulk’ fabric developed within the diamicton, largely ignoring the potential for several phases of fabric development within these typically polydeformed deposits. We present a new graphical method for the identification, description and analysis of clast microfabrics in polydeformed tills. This method utilises high resolution digital scans of orientated thin sections imported into a standard computer graphics package to measure the orientation of long axes of detrital (skeleton) grains included within the till. These data are then used to identify the main clast microfabrics present within the till, allowing the delineation of clast microfabric domains in which elongate grains share a similar preferred orientation. This process leads to the identification, characterisation and, most importantly, the interrelationships between the various generations of microfabrics. The relationships between these clast microfabrics and other microstructures (e.g. plasmic fabrics, turbate structures, shears, folds, faults…etc) can also be examined, providing a detailed microfabric-microstructural map of the thin section. Clast long axis orientation data collected for different parts of a thin section are plotted on a series of rose diagrams allowing the variation in clast microfabric orientation to be displayed graphically. A new set of terminology for the description of clast microfabrics in tills, which is based upon the system used by metamorphic petrologists, is also presented. Three case studies of the fabrics present within subglacial sediments of Pleistocene age as well as the present are used as examples of how to apply this methodology.udud
机译:尽管已使用综合的岩屑宏观和微观结构研究来提供古冰流向的证据,以区分沉积在不同沉积环境中的敌敌畏并模拟耕层对冰川下变形的响应,但此类研究通常仅检查了“散装”织物在双子叶植物内部发展,而在很大程度上忽略了这些典型的多变形沉积物中织物发展的几个阶段的潜力。我们提出了一种新的图形化方法,用于识别,描述和分析多变形耕作中的碎屑微织物。该方法利用高分辨率数字化扫描的定向薄片的数字化扫描,将其导入标准计算机图形软件包中,以测量耕作中包含的碎屑(骨架)晶粒长轴的取向。然后,这些数据将用于识别耕作中存在的主要碎屑微织物,从而勾勒出其中细长晶粒共享相似优选取向的碎屑微织物域。这个过程导致了鉴定,表征,最重要的是,导致了不同世代的微型织物之间的相互关系。还可以检查这些金属薄片微结构与其他微结构之间的关系(例如,质构织物,湍流结构,剪切,褶皱,断层等),从而提供薄截面的详细微结构图。在一系列玫瑰图中绘制了针对薄截面的不同部分收集的碎裂长轴方向数据,从而可以以图形方式显示敲击微织物方向的变化。还介绍了一套新的术语,用于描述耕层中的细微微结构,该术语基于变质岩石学家使用的系统。关于更新世时期冰川下沉积物中以及目前存在的织物的三个案例研究用作如何应用此方法的示例。 ud ud

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