The Quaternary geology of the North Sea basin
The Quaternary geology of the North Sea basin
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北海盆地第四纪地质
DOI：
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发表时间：
2017
期刊：
影响因子：
--
通讯作者：
A. Emery
中科院分区：
文献类型：
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作者：
E. Phillips;D. Hodgson;A. Emery
北海是一个浅的海湾（深50-400米），宽500公里，将英国与斯堪的纳维亚半岛和北方欧洲分开（图1）。这一陆缘陆架区有着漫长而复杂的地质历史，其现今的构造形态主要是侏罗纪-早白垩世裂谷作用以及随后的热沉降作用的结果（Glennie和Underhill，1998年; Zanella和Coward，2003年）。自中新生代以来，北海盆地中央地堑区已积累了3000米的渐新世至全新世沉积物，其中局部包括800米以上的第四纪沉积物（卡斯顿，1977年，1979年; Gatliff等人，1994年）。虽然详细了解沉积历史记录的沉积序列尚未完全建立，这些沉积物保存的证据，在不同的时间从邻近的陆地进入北海的几个冰盖的进步和退缩在第四纪。这些冰块不仅导致了周期性的侵蚀，而且对盆地的填充物也做出了重大的沉积贡献。
The North Sea is a shallow (∼50–400 m deep), ∼500-km-wide marine embayment that separates the UK from Scandinavia and northern Europe (Fig. 1). This epicontinental shelf area has had a long and complex geological history with its present-day structural configuration largely being the result of rifting during the Jurassic–Early Cretaceous, followed by thermal subsidence (Glennie and Underhill, 1998; Zanella and Coward, 2003). Since the middle Cenozoic, the Central Graben region of the North Sea basin has accumulated up to 3000 m of Oligocene to Holocene sediments, which locally includes more than 800 m of Quaternary sediments (Caston, 1977, 1979; Gatliff et al., 1994). Although a detailed understanding of the depositional history recorded by this sedimentary succession is yet to be fully established, these sediments preserve evidence for the advance and retreat of several ice sheets into the North Sea from the adjacent landmasses at different times during the Quaternary. These ice masses not only resulted in periodic erosion, but also made a significant depositional contribution to the infill of the basin.
德国亚斯蒙德半岛（吕根岛东北部）与大规模冰川运动相关的变形冰川沉积物的 3D 微观结构
影响因子：
2.3
作者：
Gehrmann;Hüneke;Meschede;Phillips
通讯作者：
Phillips
影响因子：
2.8
作者：
Sturt F
通讯作者：
Sturt F