Kamnik Savinja阿尔卑斯山脉东部最后一次更新世冰川盛期的痕迹

Q4 Social Sciences

Dela Pub Date : 2017-12-30 DOI:10.4312/DELA.47.5.127-141

Borut Stojilković

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引用次数: 1

摘要

在末次更新世极大期(LGM)，坎尼克-萨维加阿尔卑斯东部地区发生了冰川作用。对先前研究人员提到的冰川地貌和该地区的其他地貌进行了检查，绘制了地貌图，进行了形态学和形态计量学分析，并绘制了一幅新的LGM范围图。研究揭示了该地区的几个冰川，它们的大小不同，主要取决于斜坡的倾斜方向。

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The traces of the last pleistocene glacial maximum in the eastern Kamnik-Savinja Alps

The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacial Maximum (LGM). The glacial landforms mentioned by the previous researchers and other landforms in the area were examined, gemorphologically mapped, morphographically and morphometrically analysed and a new map of the extent of the LGM was produced. The research revealed several glaciers in the area and that their sizes differed, primarily depending on the slope inclination direction.

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来源期刊

Dela Social Sciences-Geography, Planning and Development

CiteScore

0.60

自引率

0.00%

发文量

审稿时长

12 weeks