The methodology of kineto-stratigraphy as applied to glacial geology
The methodology of kineto-stratigraphy as applied to glacial geology
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运动地层学方法应用于冰川地质学
DOI：
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发表时间：
1978
影响因子：
1.2
通讯作者：
A. Berthelsen
中科院分区：
文献类型：
--
作者：
A. Berthelsen
对丹麦东南部扭曲漂移层序的研究融合了冰川构造学和岩石地层学的工作方法和原理，形成了一种新的地层学--运动地层学，其中主要侧重于反映前冰盖运动模式(动力学)的定向元素的研究。通过对主要地点的研究，发现了一次以上冰川推进的沉积和变形，建立了区域动地层漂移单位，并对当地冰川沉积进行了相应的分类。讨论了各种定向元素的相对意义，并概述了丹麦东南部新的魏氏运动地层学。
Studies of contorted drift sequence in southeastern Denmark have resulted in a fusion of the working methods and principles of glacial-tectonics and lithostratigraphy and in the formulation of a new type of stratigraphy, kineto-stratigraphy, where main emphasis is placed on the study of the directional elements that reflect the movement patterns (kinetics) of former ice sheets. Through studies of principal localities, where deposits and deformation from more than one glacial advance are found, regional kinetostratigraphic drift units are established, and local glacial deposits are classified accordingly. The relative significance of the various directional elements is discussed, and a brief outline of the new Weichselian kineto-stratigraphy of southeastern Denmark is given.