Jurassic extension and Cenozoic inversion tectonics in the Asturian Basin, NW Iberian Peninsula: 3D structural model and kinematic evolution

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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 Uzkeda^a ; ^{hodei@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author} ; Mayte Bulnes^a ; ^{maite@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author} ; Josep Poblet^a ; ^{jpoblet@geol.uniovi.es" class="auth_mail" title="E-mail the corresponding author} ; José ; Carlos Garcí ; a-Ramos^b ; ^{jcgramos.muja@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; Laura Piñ ; uela^b ; ^{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

class="label">•: Middle Jurassic normal faulting, high heat flow and basin uplift caused doming.
class="label">•: Increment in the normal faults displacement during Jurassic-Cretaceous.
class="label">•: Cenozoic contraction led to buttressing, fault reactivation and new folds and thrusts.
class="label">•: The Middle Jurassic event could be a precursor of the Bay of Biscay opening.
class="label">•: The Cenozoic event caused Cantabrian ranges uplift and Bay of Biscay partial closure.

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