Discussion of 'Metamorphic P-T and retrograde path of high-pressure Barrovian metamorphic zones near Cairn Leuchan, Caledonian orogen, Scotland'
Discussion of 'Metamorphic P-T and retrograde path of high-pressure Barrovian metamorphic zones near Cairn Leuchan, Caledonian orogen, Scotland'
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关于“苏格兰加里东造山带 Cairn Leuchan 附近高压 Barrovian 变质带的变质 P-T 和逆行路径”的讨论
DOI：
10.1017/s001675681300099x
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发表时间：
2014
影响因子：
2.3
通讯作者：
Omori. S.
中科院分区：
文献类型：
--
作者：
Aoki;K.;Windley;B. F.;Maruyama;S.;Omori. S.
D.R.Viete，G.J.H.Oliver和S.A.Wilde评论：首先，我们要赞扬青木等人。(2013)一篇认真研究和发人深省的手稿。他们将巴罗维亚变质作用解释为一种根本上的逆行特征，为更传统的“峰-变质”模型提供了一种令人耳目一新的选择。
D. R. Viete, G. J. H. Oliver and S. A. Wilde comment: First, we would like to commend Aoki et al. (2013) on a careful study and thought-provoking manuscript. Their interpretation of the Barrovian metamorphism as a fundamentally retrograde feature offers a refreshing alternative to the more conventional ‘peak-metamorphic’ models.