THE DEVENSIAN MAXIMUM ICE LIMIT IN THE VALE OF YORK
THE DEVENSIAN MAXIMUM ICE LIMIT IN THE VALE OF YORK
复制标题
约克谷德文西亚最大冰限
DOI：
10.1144/pygs.40.4.631
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发表时间：
1975
影响因子：
2.8
通讯作者：
G. Gaunt
中科院分区：
文献类型：
--
作者：
G. Gaunt
从塞尔比附近向东南延伸到阿克塞姆岛南部的小型不连续的砂和砾石沉积物，根据其岩性、地层背景和地形表现，被认为是亨伯湖高水位阶段由延伸到约克谷东南部的德文斯冰舌形成的冰边缘沉积物。
Summary Small discontinuous deposits of sand and gravel extending south-east from near Selby to the southern part of the Isle of Axholme are, on the basis of their lithology, stratigraphic context and topographic expression, considered to be ice-marginal sediments formed in the high-level phase of Lake Humber by a tongue of Devensian ice which extended into the south-eastern part of the Vale of York.