《苏格兰地质学杂志》,5499-114

IF 0.5 4区 地球科学 Q4 GEOLOGY
R. Arosio, J. Howe
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引用次数: 0

摘要

本文中发现了两个错误。正确的文本如下所示。第1042页第18行:“3.664+105 cal ka BP”应为“3.664+0.105 cal ka BP’。第1112页第2行:“全新世晚期”应更正为“全新世早期”
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Erratum for ‘Lateglacial to Holocene palaeoenvironmental change in the Muck Deep, offshore western Scotland’ Scottish Journal of Geology, 54, 99-114
Two errors have been identified in this paper. The correct text is noted below. page 104 2nd col line 18: ‘3.664 + 105 cal ka BP’ should be ‘3.664 + 0.105 cal ka BP’. page 111 2nd col line 2: ‘late Holocene’ should be corrected to ‘early Holocene
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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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