Analog Models of Fold-and-Thrust Wedges in Progressive Arcs: A Comparison With the Gibraltar Arc External Wedge
| العنوان: | Analog Models of Fold-and-Thrust Wedges in Progressive Arcs: A Comparison With the Gibraltar Arc External Wedge |
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| المؤلفون: | Ana Crespo-Blanc, Juan Carlos Balanyá, Inmaculada Expósito, Alejandro Jiménez-Bonilla, Manuel Díaz-Azpiroz |
| المساهمون: | Junta de Andalucía, Ministerio de Ciencia e Innovación (España), Crespo-Blanc, Ana [0000-0003-3723-2529], Crespo-Blanc, Ana |
| المصدر: | Digital.CSIC. Repositorio Institucional del CSIC instname Frontiers in Earth Science, Vol 8 (2020) Digibug. Repositorio Institucional de la Universidad de Granada |
| بيانات النشر: | Frontiers Media, 2020. |
| سنة النشر: | 2020 |
| مصطلحات موضوعية: | strain partitioning, 010504 meteorology & atmospheric sciences, Geometry, Thrust, 010502 geochemistry & geophysics, Block rotation, 01 natural sciences, Wedge (geometry), Thin-skinned tectonics, progressive arc, Arc (geometry), Analog model, Progressive arc, Clockwise, lcsh:Science, 0105 earth and related environmental sciences, Fold (geology), block rotation, analog model, Tectonics, Strain partitioning, Analogue modelling, Gibraltar Arc external wedge, thin-skinned tectonics, General Earth and Planetary Sciences, lcsh:Q, Geology |
| الوصف: | The timing and kinematics of the different types of structures and the associated vertical-axis rotations that permit an arcuate external wedge to acquire progressively its curved shape throughout its deformation history—known as progressive arcs—are key questions in natural cases of arcuate fold-and-thrust belts that we want to address through analog modeling. We present laboratory models of fold-and-thrust belts formed with a backstop that deforms in map view to simulate progressive arcs in a thin-skinned tectonic regime. Our setup makes use of a deformable backstop rigid enough to push from behind the initial parallelepiped but deformable in map view. This innovative design permits us to increase the amplitude of the arc indenting in the model as its radius of curvature decreases, that is, it simulates a progressive arc. Taking the Gibraltar Arc external wedge situated in the western Mediterranean to scale our models in terms of rheology, velocities, and sizes, four types of experiments were made. We varied the type of substratum (sand or silicone), the silicone thickness, and the width and length of the initial analog pack in order to test the influence of each of these parameters on the resulting fold-and-thrust belts. All experiments led to the formation of arcuate wedges where strain was partitioned into: (a) arc-perpendicular shortening, accommodated by thrusts which main structural trend is broadly subparallel to the indenter shape and with divergent transport directions, and (b) arc-parallel stretching, accommodated by normal and conjugate strike-slip faults. The normal and strike-slip faults contributed to the fold-and-thrust belt segmentation and the formation of independent blocks that rotated clockwise and counterclockwise depending on their position within the progressive arc. Our experiments allow to simulate and understand the finite deformation mode of the external wedge of the Gibraltar Arc. Accordingly, they shed light on how an arcuate fold-and-thrust belt can develop progressively in terms of structural trend and transport directions, types and distribution of the structures accommodating strain partition, and timing of vertical-axis rotations. This study was supported by projects RNM-0451, EST1/00231, CGL2017-89051-P, PGC2018-100914-B-I00, and UPO 1259543. |
| تدمد: | 2017-8905 |
| URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_dedup___::34b8818a0c468972d0c7c2984b0ead22 http://hdl.handle.net/10261/213855 |
| Rights: | OPEN |
| رقم الانضمام: | edsair.doi.dedup.....34b8818a0c468972d0c7c2984b0ead22 |
| قاعدة البيانات: | OpenAIRE |
| تدمد: | 20178905 |
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