Experimental frost shattering
Experimental frost shattering
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DOI：
10.1177/030913338200600202
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发表时间：
1982-06
期刊：
影响因子：
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通讯作者：
J. Lautridou;J. Ozouf
中科院分区：
文献类型：
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作者：
J. Lautridou;J. Ozouf
在过去的15年中，法国卡昂CNRS Gdomorphologie中心进行了大量的研究，重点是研究实验室模拟霜冻对不同岩石类型的影响。我们的公报和各种法文期刊都详细记录了这项工作的结果。然而，不幸的是，这些发现并没有通过地貌学文献的一般机构有效地传播。在人们对冰缘过程及其影响越来越感兴趣的时候，对我们的一些更重要的发现提供一个简短的英语摘要可能是有用的。故意避免提及英文参考资料。我们知道在其他国家进行的大部分研究（Lautridou，1978; Lautridou和McGreevy，1980），并在我们以前发表的工作中讨论了我们与其他人的研究结果。没有这样的讨论，
During the past fifteen years a considerable amount of the research conducted at the Centre de Gdomorphologie du CNRS, Caen, France, has focused on examining the effects of laboratory-simulated frost shattering on different rock types. The results of this work have been well documented in our Bulletins and in various French-language journals. Unfortunately, however, these findings have not been effectively disseminated through the general body of geomorphological literature. At a time when there appears to be a growing interest in periglacial processes and their effects, it may prove useful to provide a short English-language summary of some of our more significant findings. Mention of English-language references has been deliberately avoided. We are aware of most of the research which has been carried out in other countries (Lautridou, 1978; Lautridou and McGreevy, 1980), and have discussed our findings in relation to those of others in our previously published work. No such discussion is