波兰南部地质生态系统中间冰期气候变化的反映

GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series Pub Date : 2016-01-01 DOI:10.4316/GEOREVIEW.2016.0.0.337

D. Michczyńska

{"title":"波兰南部地质生态系统中间冰期气候变化的反映","authors":"D. Michczyńska","doi":"10.4316/GEOREVIEW.2016.0.0.337","DOIUrl":null,"url":null,"abstract":"The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits","PeriodicalId":30470,"journal":{"name":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","volume":"233 1","pages":"60"},"PeriodicalIF":0.0000,"publicationDate":"2016-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland\",\"authors\":\"D. Michczyńska\",\"doi\":\"10.4316/GEOREVIEW.2016.0.0.337\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits\",\"PeriodicalId\":30470,\"journal\":{\"name\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"volume\":\"233 1\",\"pages\":\"60\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2016-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.4316/GEOREVIEW.2016.0.0.337\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.4316/GEOREVIEW.2016.0.0.337","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}

引用次数: 0

摘要

在最后一个寒冷期，欧洲中部被永久冻土带占据，并被斯堪的纳维亚冰盖两次入侵，但大约70%的时间被永久冻土带连续波动的过渡阶段所占据，这主要反映在斜坡、河流和风成沉积物的类型和厚度上

本文章由计算机程序翻译，如有差异，请以英文原文为准。

查看原文本刊更多论文

Reflection of climatic changes during Interpleniglacial in geoecosystems of Southern Poland

The central part of Europe during the last cold stage was occupied by permafrost and twice invaded by the Scandinavian ice sheet, but about 70% of time was taken by transitional phases of continuous fluctuations of permafrost, which are reflected especially in type and thickness of slope, fluvial and aeolian deposits

求助全文

通过发布文献求助，成功后即可免费获取论文全文。去求助

来源期刊

GEOREVIEW Scientific Annals of Stefan cel Mare University of Suceava Geography Series

自引率

0.00%

发文量

审稿时长

6 weeks