{"title":"波罗的海东部冰湖的形成时间","authors":"J. Vassiljev, L. Saarse","doi":"10.17741/BGSF/85.1.001","DOIUrl":null,"url":null,"abstract":"A shoreline database for the Baltic, covering the Late Weichselian and Holocene, was compiled. The database includes about 1600 sites from Estonia, Latvia, Lithuania, Finland, NW Russia, Poland, Sweden and was used to create a GIS-based palaeogeographical reconstructions on the development of the Baltic Ice Lake (BIL). The formation of the highest shoreline of the BIL in Estonia was connected with the development of the Pandivere ice marginal zone (Estonia) and the lowest with the Salpausselka ice-marginal formations (Finland). There was a well-accepted knowledge that the Pandivere ice marginal zone correlates with the Neva ice marginal zone in NW Russia dated to 13 300 cal yr BP. Recent studies of the late glacial sites in northern Estonia indicate that the age of the Pandivere ice marginal zone and hence the highest shoreline of the BIL A 1 is about 13 800–14 000 cal yr BP. It was followed by the BIL stage A 2 , which formed in front of the Palivere ice marginal belt about 13 200–13 500 cal yr BP. The final drainage of the BIL took place about 11 650 cal yr BP. The timing of the BIL stages was derived from AMS- 14 C dates and correlated with varve chronology, OSL and 10 Be dates.","PeriodicalId":55302,"journal":{"name":"Bulletin of the Geological Society of Finland","volume":null,"pages":null},"PeriodicalIF":1.3000,"publicationDate":"2013-06-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"35","resultStr":"{\"title\":\"Timing of the Baltic Ice Lake in the eastern Baltic\",\"authors\":\"J. Vassiljev, L. Saarse\",\"doi\":\"10.17741/BGSF/85.1.001\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A shoreline database for the Baltic, covering the Late Weichselian and Holocene, was compiled. The database includes about 1600 sites from Estonia, Latvia, Lithuania, Finland, NW Russia, Poland, Sweden and was used to create a GIS-based palaeogeographical reconstructions on the development of the Baltic Ice Lake (BIL). The formation of the highest shoreline of the BIL in Estonia was connected with the development of the Pandivere ice marginal zone (Estonia) and the lowest with the Salpausselka ice-marginal formations (Finland). There was a well-accepted knowledge that the Pandivere ice marginal zone correlates with the Neva ice marginal zone in NW Russia dated to 13 300 cal yr BP. Recent studies of the late glacial sites in northern Estonia indicate that the age of the Pandivere ice marginal zone and hence the highest shoreline of the BIL A 1 is about 13 800–14 000 cal yr BP. It was followed by the BIL stage A 2 , which formed in front of the Palivere ice marginal belt about 13 200–13 500 cal yr BP. The final drainage of the BIL took place about 11 650 cal yr BP. The timing of the BIL stages was derived from AMS- 14 C dates and correlated with varve chronology, OSL and 10 Be dates.\",\"PeriodicalId\":55302,\"journal\":{\"name\":\"Bulletin of the Geological Society of Finland\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":1.3000,\"publicationDate\":\"2013-06-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"35\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Bulletin of the Geological Society of Finland\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.17741/BGSF/85.1.001\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"GEOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Bulletin of the Geological Society of Finland","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.17741/BGSF/85.1.001","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOLOGY","Score":null,"Total":0}
引用次数: 35
摘要
编制了一个涵盖晚魏奇塞利世和全新世的波罗的海海岸线数据库。该数据库包括来自爱沙尼亚、拉脱维亚、立陶宛、芬兰、俄罗斯西北部、波兰和瑞典的约1600个地点,并用于创建基于gis的波罗的海冰湖(BIL)发展的古地理重建。爱沙尼亚境内BIL最高岸线的形成与Pandivere冰边缘带(爱沙尼亚)的发育有关,最低岸线的形成与Salpausselka冰边缘带(芬兰)的发育有关。Pandivere冰边缘带与俄罗斯西北部的涅瓦河冰边缘带的历史可追溯到13300 calyr BP,这是一个公认的认识。最近对爱沙尼亚北部晚冰期遗址的研究表明,Pandivere冰边缘带的年龄约为13 800-14 000 calyr BP。其后是在13 200 ~ 13 500 cal yr BP左右形成于Palivere冰边缘带前的BIL阶段a2。BIL的最终排水发生在11650 calybp左右。BIL分期的时间由AMS- 14c数据得出,并与瓣膜年代学、OSL和10be数据相关。
Timing of the Baltic Ice Lake in the eastern Baltic
A shoreline database for the Baltic, covering the Late Weichselian and Holocene, was compiled. The database includes about 1600 sites from Estonia, Latvia, Lithuania, Finland, NW Russia, Poland, Sweden and was used to create a GIS-based palaeogeographical reconstructions on the development of the Baltic Ice Lake (BIL). The formation of the highest shoreline of the BIL in Estonia was connected with the development of the Pandivere ice marginal zone (Estonia) and the lowest with the Salpausselka ice-marginal formations (Finland). There was a well-accepted knowledge that the Pandivere ice marginal zone correlates with the Neva ice marginal zone in NW Russia dated to 13 300 cal yr BP. Recent studies of the late glacial sites in northern Estonia indicate that the age of the Pandivere ice marginal zone and hence the highest shoreline of the BIL A 1 is about 13 800–14 000 cal yr BP. It was followed by the BIL stage A 2 , which formed in front of the Palivere ice marginal belt about 13 200–13 500 cal yr BP. The final drainage of the BIL took place about 11 650 cal yr BP. The timing of the BIL stages was derived from AMS- 14 C dates and correlated with varve chronology, OSL and 10 Be dates.
期刊介绍:
Bulletin of the Geological Society of Finland (BGSF) publishes research articles and short communications in all branches of geosciences. Contributions from outside Finland are welcome, provided that they contain material relevant to Finnish geology or are of general interest.