Jurassic extension and Cenozoic inversion tectonics in the Asturian Basin, NW Iberian Peninsula: 3D structural model and kinematic evolution
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- 作者：Hodei Uzkedaa ; hodei@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author ; Mayte Bulnesa ; maite@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author ; Josep Pobleta ; jpoblet@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author ; José ; Carlos Garcí ; a-Ramosb ; jcgramos.muja@gmail.com" class="auth_mail" title="E-mail the corresponding author ; Laura Piñ ; uelab ; lpinuela.muja@gmail.com" class="auth_mail" title="E-mail the corresponding author
- 关键词：Normal fault ; Reverse fault ; Reactivated fault ; Inversion tectonics ; Basin inversion ; Jurassic ; Asturian Basin
- 刊名：Journal of Structural Geology
- 出版年：2016
- 出版时间：September 2016
- 年：2016
- 卷：90
- 期：Complete
- 页码：157-176
- 全文大小：8076 K
文摘
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Middle Jurassic normal faulting, high heat flow and basin uplift caused doming.
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Increment in the normal faults displacement during Jurassic-Cretaceous.
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Cenozoic contraction led to buttressing, fault reactivation and new folds and thrusts.
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The Middle Jurassic event could be a precursor of the Bay of Biscay opening.
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The Cenozoic event caused Cantabrian ranges uplift and Bay of Biscay partial closure.