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首页> 外文期刊>Geological Quarterly >Texture and petrography of glacial deposits in the northern foothill of the Hruby Jesenik and Rychlebske Mts., Czechia
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Texture and petrography of glacial deposits in the northern foothill of the Hruby Jesenik and Rychlebske Mts., Czechia

机译:捷克Hruby Jesenik山和Rychlebske山北麓的冰川沉积物的质地和岩石学

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摘要

The petrographic and mineralogical characteristics of glacial deposits from the localities in the northern foothills of the Hruby Jesenik and Rychlebske Mts. have been studied. Grain-size, petrographic composition, heavy minerals, clast shape and roundness have been investigated. The data obtained have been used to create a probability model to differentiate the stratigraphy of particular accumulations and for partial reconstruction of the advance direction of the ice sheet in the area. The main advance direction of the ice sheet was presumed to be from the NW to SE in this region. The erratic material was probably predominantly transported in the basal ice layers according to the clast shape and roundness. An Elsterian age of the sedimentary bodies investigated is suggested by correlation with analogous deposits in adjacent parts of Poland. This model contradicts previous correlations. However, further constraints on the stratigraphic position of these deposits would require the application of dating techniques.
机译:Hruby Jesenik和Rychlebske山北部山麓地区的冰川沉积物的岩石学和矿物学特征。已经研究过了。研究了晶粒大小,岩石学组成,重矿物,碎屑形状和圆度。获得的数据已用于创建概率模型,以区分特定堆积物的地层学,并用于部分重建该地区冰盖的前进方向。假定该区域冰盖的主要前进方向是从西北到东南。根据岩屑的形状和圆度,不稳定的物质可能主要在基底冰层中运输。通过与波兰邻近地区的类似沉积物的相关性,表明了所研究沉积体的埃尔斯特时代。该模型与先前的相关性矛盾。但是,对这些矿床地层位置的进一步限制将要求应用测年技术。

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