Reply to Discussion on ‘The Neoproterozoic to Mid-Devonian evolution of Scotland: a review and unresolved issues’ Scottish Journal of Geology, 51, 5–30
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引用次数: 1
Abstract
In the first paragraph of his discussion of our paper, Burton sets up his definition of what he thinks should have been the structure and purpose of our paper, his opinion of what a review should be and then complains that we did not follow his definition. We reject his definition, having defined our purpose in the abstract of our review. We were invited to write a short review of the Precambrian–Lower Palaeozoic tectonic history of Scotland. We structured the review around the topics that interest us; the paper was not, and could not be, an in-depth review of the opinion of everyone who had published relevant data and ideas on the topics covered in the paper. Our purpose, in the space allotted, was to present an overview review rather than a lengthy document argued in detail with references to everyone who had published on the topic. A full detailed analysis and review of the kind suggested would have been far too long for the Scottish Journal of Geology. The purpose of the paper is stated in the abstract and the last paragraph of the summary. There was no conscious effort to exclude Bluck's work; his work did not feature in our review, just as that of many hundreds of geologists who have also written on the subject. Several people who reviewed the manuscript, including the referees, made no mention of the absence of references to Bluck's published work, and it simply did not occur to us as we wrote it. We regret that this has caused offence. In our short review, we outlined our views and did not try to include and argue against all the different opinions with which we disagree. To have done so would have quadrupled the reference list and at least doubled the length of the paper. The whole Highland Border issue has been argued interminably for ages (often in the Scottish Journal of Geology) and, in the end, the consensus was against Bluck's views (e.g. Henderson et al. 2009). There is no point in bringing up arguments just to shoot them down; we do not see that as a positive legacy to Bluck, whose work in fluvial sedimentology was superb.
在他讨论我们的论文的第一段,伯顿建立了他的定义,他认为应该是我们的论文的结构和目的,他的意见应该是什么审查,然后抱怨我们没有遵循他的定义。我们拒绝他的定义,因为我们已经在综述的摘要中定义了我们的目的。我们应邀写了一篇关于苏格兰前寒武纪-下古生代构造史的简短综述。我们围绕我们感兴趣的主题来组织评论;这篇论文不是,也不可能是对所有发表过相关数据和观点的人的意见的深入审查。在指定的篇幅内,我们的目的是提出一份概括性的评论,而不是一份冗长的文件,详细讨论每个在该主题上发表过文章的人。对于《苏格兰地质学杂志》来说,对这类建议进行全面详细的分析和回顾太长了。摘要和结束语的最后一段阐述了本文的目的。他们并没有刻意排斥布莱克的作品;他的工作没有出现在我们的评论中,就像成百上千的地质学家一样,他们也写了关于这个主题的文章。几位审阅过手稿的人,包括评审人,都没有提到没有参考布鲁克已发表的作品,我们在写手稿的时候根本没有想到这一点。我们很遗憾这引起了冒犯。在我们简短的评论中,我们概述了我们的观点,并没有试图包括和反对我们不同意的所有不同意见。如果这样做的话,参考文献的数量会增加四倍,论文的长度至少会增加一倍。整个高地边界问题已经争论了很多年了(通常在苏格兰地质学杂志上),最后,共识是反对Bluck的观点(例如Henderson et al. 2009)。提出争论只是为了驳倒它们是没有意义的;我们不认为这是对布鲁克的积极遗产,他在河流沉积学方面的工作是一流的。
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.