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首页> 外文期刊>Contributions to Mineralogy and Petrology >Comment to paper: Timing of magmatism and metamorphism in the Gruinard Bay area of the Lewisian gneiss complex: comparison with the Assynt Terrane and implications for terrane accretion by G.J. Love, P.D. Kinny and C.R.L. Friend
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Comment to paper: Timing of magmatism and metamorphism in the Gruinard Bay area of the Lewisian gneiss complex: comparison with the Assynt Terrane and implications for terrane accretion by G.J. Love, P.D. Kinny and C.R.L. Friend

机译:对文件的评论:刘易斯片麻岩复合体格鲁纳德湾地区的岩浆作用和变质作用的时机:与Assynt地形的比较及其对G.J.爱,博士Kinny和C.R.L.友人

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摘要

The paper by Love et al. (2004) (in the following abbreviated to L04 for convenience) reports an interesting set of U-Pb data for units of the Lewisian Complex at Badcall Bay, Lochinver and Gruinard Bay in northern Scotland, expanding our understanding of the geological relationships in the Complex and also providing new insights on the systematics of zircon in high-grade rocks. Besides the many positive points the paper, however, contains some dubious interpretations that ignore or misrepresent available evidence. This comment addresses some of these points, rectifies some twisted quotations and answers some technical remarks.
机译:Love等人的论文。 (2004年)(为方便起见,以下简称L04)报告了苏格兰北部Badcall湾,Lochinver和Gruinard湾刘易斯综合体单元的一组有趣的U-Pb数据,扩大了我们对该综合体中地质关系的理解并提供有关高档岩石中锆石系统的新见解。但是,除了许多积极的观点外,本文还包含一些可疑的解释,这些解释忽略或错误地代表了现有证据。该评论解决了其中的一些问题,纠正了一些错误的引用,并回答了一些技术性的评论。

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