Structure of the (ultra)high-pressure Western Gneiss Region, Norway: Imbrication during Caledonian continental margin subduction

Structure of the (ultra)high-pressure Western Gneiss Region, Norway: Imbrication during Caledonian continental margin subduction
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挪威西部(超)高压片麻岩地区的结构:加里东大陆边缘俯冲期间的叠瓦

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发表时间:
2017
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通讯作者:
D. Young
D. Young
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作者:
D. Young

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