首页> 外文期刊>Arctic: Journal of the Arctic Institute of North America >Late Weichselian glacial geology of the lower Borgarfj?rdur region, western Iceland : a preliminary report
【24h】

Late Weichselian glacial geology of the lower Borgarfj?rdur region, western Iceland : a preliminary report

机译:冰岛西部下博尔菲菲尔-德杜尔地区的魏氏后期冰川地质:初步报告

获取原文
           

摘要

Morphological and lithostratigraphical investigations have revealed two successive glacial advances of Late Weichselian age in the lower Borgarfj?rdur region, Western Iceland. Studies of the Melabakkar-ásbakkar coastal cliffs have disclosed a complex of glaciomarine sediments and tills, accompanied by glaciofluvial deposits from ice marginal sources. A brief description is given for each of the major lithostratigraphical units, and a depositional model for the sequence is outlined. The first glacial advance occurred some time shortly after 12 000 radiocarbon years before present (BP), and the second one around 11 000 BP. By 10 000 BP the glaciers had retreated from the lowlands and the sea transgressed to 60 m above present sea level, where extensive marine terraces were formed
机译:形态学和岩石地层学调查表明,在冰岛西部较低的Borgarfj?rdur地区,魏氏时代晚期有两次连续的冰川发展。对Melabakkar-ásbakkar沿海悬崖的研究表明,冰川海洋沉积物和耕till物复杂,并伴有来自冰边缘来源的冰川河流沉积物。对每个主要岩相地层学单位进行了简要说明,并概述了该层序的沉积模型。第一次冰川发展发生在距今12,000放射性碳年(BP)之后不久的一段时间,第二次冰川发展约为11000 BP。到10000 BP时,冰川已从低地撤退,海面越过了现在的海平面60 m,形成了广阔的海洋阶地

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号