Strain partitioning into dry and wet zones and the formation of Ca-rich myrmekite in syntectonic syenites: A case for melt-assisted dissolution-replacement creep under granulite facies conditions
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- 作者：G.B. De Tonia ; gdetoni@ufrgs.br" class="auth_mail" title="E-mail the corresponding author ; M.F. Bitencourta ; b ; L.V.S. Nardia ; b
- 关键词：Syntectonic magmatism ; Syntectonic syenites ; Myrmekite ; Dissolution-replacement creep ; Strain partitioning ; Granulite facies conditions
- 刊名：Journal of Structural Geology
- 出版年：2016
- 出版时间：October 2016
- 年：2016
- 卷：91
- 期：Complete
- 页码：88-101
- 全文大小：8454 K
文摘
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Pervasive myrmekite formation by coupled deformation and late-magmatic liquid inflow.
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Pervasive Ca-rich myrmekite formation reported in syntectonic syenites.
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Dissolution-replacement creep may be effective under granulite facies conditions.
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Strain partitioning into dry and wet zones in granulite facies environments.