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首页> 外文期刊>Doklady Earth Sciences >Geological-Stratigraphic Position of Upper Pleistocene Marine Sediments in the Southern Kola Peninsula: Evidence from Geochronological and Geological Data
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Geological-Stratigraphic Position of Upper Pleistocene Marine Sediments in the Southern Kola Peninsula: Evidence from Geochronological and Geological Data

机译:科拉半岛南部上更新世海洋沉积物的地质-地质位置:来自年代学和地质数据的证据

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摘要

The presented analytical data specify the geological -stratigraphic position of interglacial sequences that serve as important geological and paleogeographic markers. Solution of this problem is of theoretical and paleogeographic significance in the correlation of Late Pleistocene events in different regions and prospecting for diamond and other mineral placers. The works were carried out in the western Terskii Coast of the White Sea, where differently aged interglacial sediments are exposed along the steep slopes of river valleys. Collected samples were dated using the electron spin resonance (ESR) and optically stimulated luminescence (OSL) methods, which made it possible to specify the geological-stratigraphic position of interglacial marine sedimentary units.
机译:提出的分析数据说明了冰川间层序的地质-地层位置,它们是重要的地质和古地理标志。该问题的解决在不同地区晚更新世事件的相关性以及钻石和其他矿物砂矿的勘探方面具有理论和古地理意义。这项工作是在白海的Terskii西部海岸进行的,那里沿河谷的陡坡暴露了不同年龄的冰川间沉积物。使用电子自旋共振(ESR)和光激发发光(OSL)方法对收集的样品标出了日期,这使得确定冰间海洋沉积单元的地质地层位置成为可能。

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