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Pleistocene and Holocene aeolian sediments of different location and geological history: A new insight from rounding and frosting of quartz grains

机译:不同位置和地质历史的更新世和全新世风沙沉积:石英颗粒的修圆和磨砂的新见解

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摘要

Rounding and frosting of quartz grains in aeolian sediments of the known stratigraphic position and unique geological setting was explored in Finnish, Estonian, Latvian, and Polish localities and in Fuer-teventura Island. The aim of the study is to characterize the variability of the spatial pattern of rounding and frosting of quartz grains in the sandy (0.5-0.8 mm) fraction and to evaluate the factors influencing it The relationships between rounded and non-abraded, as well as matt- and shiny-type quartz grains were calculated for 159 samples and evaluated against the aeolian subenvironment, substratum and presumed age of the locations. The obtained relations do not confirm meridional changeability of textural features previously observed in Poland and suggest a larger impact of the substratum on textural features of cold-environment aeolian sediments.
机译:在芬兰,爱沙尼亚,拉脱维亚和波兰等地以及富特-图文图拉岛地区,对已知地层位置和独特地质环境的风沙沉积物中的石英颗粒进行了修整和磨砂处理。该研究的目的是表征沙质(0.5-0.8 mm)级分中石英颗粒的倒圆和磨砂的空间格局的变化,并评估影响其的因素。倒圆与非磨砂之间的关系以及计算了159个样品的无光泽和有光泽类型的石英晶粒,并根据风沙亚环境,基底和位置的假定年龄进行了评估。所获得的关系并不能证实先前在波兰观察到的地貌特征的经向变化性,并且表明该基质对冷环境风沙沉积物的地貌特征具有更大的影响。

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  • 来源
    《Quaternary International》 |2014年第10期|311-322|共12页
  • 作者

    Edyta Kalinska; Maris Nartiss;

  • 作者单位

    Institute of Ecology and Earth Sciences, Department of Geology, Faculty of Science, University of Tartu, Ravila Str. 14A, Tartu EE50411, Estonia;

    Faculty of Geography and Earth Sciences, University of Latvia, Alberta Str. 10, Riga LV1586, Latvia;

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