Shear zone evolution and timing of deformation in the Neoproterozoic transpressional Dom Feliciano Belt, Uruguay
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- 作者：Sebastiá ; n Orioloa ; seba.oriolo@gmail.com" class="auth_mail" title="E-mail the corresponding author ; soriolo@gwdg.de" class="auth_mail" title="E-mail the corresponding author ; Pedro Oyhantç ; abalb ; Klaus Wemmera ; Florian Heidelbachc ; Jö ; rg Pfä ; nderd ; Miguel A.S. Baseie ; Mathias Huecka ; Felix Hannicha ; Blanka Spernerd ; Siegfried Siegesmunda
- 关键词：Brasiliano&ndash ; Pan-African Orogeny ; Rí ; o de la Plata Craton ; Oblique collision ; Transpression ; Strain partitioning ; Gondwana
- 刊名：Journal of Structural Geology
- 出版年：2016
- 出版时间：November 2016
- 年：2016
- 卷：92
- 期：Complete
- 页码：59-78
- 全文大小：10722 K
文摘
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Inclined transpression with temporal and spatial variations of strain.
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Shear zones record strain localization and retrograde conditions during exhumation.
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Main crustal shortening, deformation and metamorphism between 630 and 600 Ma.
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Río de la Plata-Congo collision recorded in the Dom Feliciano Belt at ca. 630 Ma.
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Orogen-parallel sinistral shearing after 600 Ma resulting from Kalahari convergence.