对Smith等人关于“苏格兰内赫布里底群岛SE Raasay冰川消融与新构造”讨论的答复,2021 (SJG, 57, 106-116)

IF 0.5 4区 地球科学 Q4 GEOLOGY
David E. Smith, C. Firth, T. Mighall, P. Teasdale
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引用次数: 0

摘要

我们非常感谢莫顿博士对我们论文的兴趣和他赞赏的评论。我们认为,对苏格兰西部这一地区的冰川消融和新构造模式感兴趣的地质学家对贝因纳利克的特征特别感兴趣。该位置在新仙女木期/全新世断层错位的量级上是苏格兰独一无二的。我们对Morton博士的评论作出如下回应:
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Reply to discussion on ‘Deglaciation and neotectonics in SE Raasay, Scottish Inner Hebrides’, by Smith et al. 2021 (SJG, 57, 106–116)
We greatly appreciate Dr Morton's interest in our paper and his appreciative comments. The features at Beinn na Leac are, in our opinion, of particular interest to geologists interested in the pattern of deglaciation and neotectonics in this part of western Scotland. The location is unique in Scotland in the magnitude of Younger Dryas/Holocene fault dislocation. We respond to Dr Morton's comments as follows:
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来源期刊
Scottish Journal of Geology
Scottish Journal of Geology 地学-地质学
CiteScore
1.70
自引率
0.00%
发文量
10
审稿时长
>12 weeks
期刊介绍: Although published only since 1965, the Scottish Journal of Geology has a long pedigree. It is the joint publication of the Geological Society of Glasgow and the Edinburgh Geological Society, which prior to 1965 published separate Transactions: from 1860 in the case of Glasgow and 1863 for Edinburgh. Traditionally, the Journal has acted as the focus for papers on all aspects of Scottish geology and its contiguous areas, including the surrounding seas. The publication policy has always been outward looking, with the Editors encouraging review papers and papers on broader aspects of the Earth sciences that cannot be discussed solely in terms of Scottish geology. The diverse geology of Scotland continues to provide an important natural laboratory for the study of earth sciences; many seminal studies in geology have been carried out on Scottish rocks, and over the years the results of much of this work had been published in the Journal and its predecessors. The Journal fully deserves its high reputation worldwide and intends to maintain its status in the front rank of publications in the Earth sciences.
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