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Loess is [almost totally formed by] the accumulation of dust

机译:黄土[几乎完全由]灰尘的堆积形成

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摘要

In 1990 Marton Pecsi published a paper entitled 'Loess is not just the accumulation of dust'. This 1990 paper presented the case for considering aspects of loess formation other than the aeolian deposition of silty material. Pecsi argued that there is more to loess formation than simply the fact of aeolian deposition. While not disputing the validity of much of Pecsi's arguments a case can be made for considering that aeolian deposition is at the very heart of loess formation, that the factor of aeolian deposition is so critical that other aspects are relatively unimportant. Pecsi appeared to suggest that aeolian deposition is just one of many factors relating to the formation of loess deposits; this is not so aeolian deposition and the consequent formation of metastable structures is absolutely central. But, it is probably useful to consider the 'aeolian deposition is absolutely critical' approach and the 'aeolian deposition is one of the factors' approach in some more detail, and in relation to each other. Some insights may accrue; interesting things do happen after the deposition of the dust and this needs to be acknowledged.
机译:1990年,马顿·佩西(Marton Pecsi)发表了一篇题为“黄土不仅仅是尘土的积累”的论文。 1990年的这篇论文提出了考虑除风沙沉积的粉质材料以外的黄土形成方面的案例。佩奇认为,黄土的形成不仅仅是风成沉积的事实。尽管没有争议许多佩奇观点的有效性,但可以考虑风成因是黄土形成的核心,但风成因非常重要,以至于其他方面都不重要。 Pecsi似乎暗示风成沉积只是与黄土沉积物形成有关的许多因素之一。这不是风沙沉积,因此亚稳结构的形成绝对是核心。但是,考虑“风成沉积是绝对关键的”方法和“风成沉积是影响因素的方法之一”可能更为有用,而且彼此之间也有关系。可能会产生一些见解;灰尘沉积后确实会发生有趣的事情,这需要得到承认。

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  • 来源
    《Quaternary International》 |2011年第2011期|p.4-11|共8页
  • 作者单位

    Giotto Loess Research Croup, Arkwright Materials Project, Nottingham Trent University, Nottingham NCI 4BU, UK;

    Chair of Physical Geography, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovica 3, 21000 Novi Sad, Serbia;

    Laboratory for Palaeoenvironmental Reconstruction, Faculty of Sciences, University of Novi Sad, Trg Dositeja Obradovica 2, 21000 Novi Sad, Serbia;

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