Turbidites and turbidity currents from Alpine ‘flysch’ to the exploration of continental margins
Turbidites and turbidity currents from Alpine ‘flysch’ to the exploration of continental margins
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DOI：
10.1111/j.1365-3091.2008.01019.x
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发表时间：
2009-01
期刊：
影响因子：
3.5
通讯作者：
E. Mutti;D. Bernoulli;F. Lucchi;R. Tinterri
中科院分区：
文献类型：
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作者：
E. Mutti;D. Bernoulli;F. Lucchi;R. Tinterri
自Kuenen和Migliorini于1950年首次定义浊积岩以来，浊积岩的概念已经发生了很大的变化，即浊流的存款，以北方亚平宁山脉的桑迪复理石序列为例，现在它被用来定义各种存款，其中一些在相、几何形状和地质意义方面与桑迪复理石地层几乎没有共同之处。将这一概念扩展到其他地球动力学背景和非硅质矿物组成的矿床，仅在结论部分作简要讨论。
The concept of turbidite has evolved so much since its original definition by Kuenen and Migliorini in 1950 – i.e. the deposit of turbidity currents exemplified by the sandy flysch successions of the Northern Apennines – that it is now used to define a variety of deposits, some of which have little in common with sandy flysch formations in terms of facies, geometry and geological significance. The extension of the concept to other geodynamic settings and deposits of non‐siliciclastic composition is considered only briefly in the concluding sections.