Structure of an inverted basin from subsurface and field data: the Late Jurassic-Early Cretaceous Maestrat Basin (Iberian Chain)

Structure of an inverted basin from subsurface and field data: the Late Jurassic-Early Cretaceous Maestrat Basin (Iberian Chain)

The Maestrat Basin experienced two main rifting events: Late Permian-Late Triassic and Late Jurassic-Early Cretaceous, and was inverted during the Cenozoic Alpine orogeny. During the inversion, an E-W-trending, N-verging fold-and-thrust belt developed along its northern margin, detached in the Tria...

Full description

Bibliographic Details
Main Authors: M. NEBOT, J.J. GUIMERÀ I ROSSO
Format: Article
Language:English
Published: Universitat de Barcelona (UB), Geociències Barcelona (Geo3BCN), Institut de Diagnosi Ambiental i Estudis de l'Aigua (IDAEA), Universitat Autònoma de Barcelona (UAB) 2016-05-01
Series:Geologica Acta
Subjects:
Basin inversion
Fault-bend fold
Vertical tectonic step
Low-dip ramp
Salt flow
Online Access:https://revistes.ub.edu/index.php/GEOACTA/article/view/13980

Internet

https://revistes.ub.edu/index.php/GEOACTA/article/view/13980

Similar Items