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Deciphering late Devonian‐early Carboniferous P‐T‐t path of mylonitised garnet‐mica schists from Prins Karls Forland, Svalbard
Journal of Metamorphic Geology ( IF 3.4 ) Pub Date : 2020-04-06 , DOI: 10.1111/jmg.12529
Karolina Kośmińska 1 , Frank S. Spear 2 , Jarosław Majka 1, 3 , Karol Faehnrich 4 , Maciej Manecki 1 , Karsten Piepjohn 5 , Winfried K. Dallmann 6
Affiliation  

This is the peer reviewed version of the following article: Kośminska, K., Spear, F. S., Majka, J., Faehnrich, K., Manecki, M., Piepjohn, K. & Dallmann, W. K. (2020). Deciphering late Devonian–early Carboniferous P–T–t path of mylonitized garnet-mica schists from Prins Karls Forland, Svalbard. Journal of Metamorphic Geology, ?(?), ?., which has been published in final form at https://doi.org/10.1111/jmg.12529 . This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.

中文翻译:

破译来自斯瓦尔巴群岛普林斯卡尔斯福兰的糜棱化石榴石云母片岩的晚泥盆世-早石炭世 P-T-t 路径

这是以下文章的同行评审版本:Kośminska, K., Spear, FS, Majka, J., Faehnrich, K., Manecki, M., Piepjohn, K. & Dallmann, WK (2020)。破译来自斯瓦尔巴群岛的普林斯卡尔斯福兰的糜棱化石榴石云母片岩的晚泥盆世-早石炭纪 P-T-t 路径。Journal of Metamorphic Geology, ?(?), ?.,已在 https://doi.org/10.1111/jmg.12529 上以最终形式发表。根据 Wiley 使用自存档版本的条款和条件,本文可用于非商业目的。
更新日期:2020-04-06
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