FN Archimer Export Format
PT J
TI Polyphase tectonic evolution of fore‐arc basin related to STEP fault as revealed by seismic reflection data from the Alboran Sea (W‐Mediterranean)
BT 
AF d'Acremont, E.
   Lafosse, M.
   Rabaute, A.
   Teurquety, G.
   Do Couto, D.
   Ercilla, G.
   Juan, C.
   Mercier de Lépinay, B.
   Lafuerza, Sara
   Galindo‐Zaldivar, J.
   Estrada, F.
   Vazquez, J.T.
   Leroy, S.
   Poort, J.
   Ammar, A.
   Gorini, C.
AS 1:1;2:1;3:1;4:1,2;5:1;6:3;7:3;8:4;9:1;10:5,6;11:3;12:7;13:1;14:1;15:8;16:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;
C1 Sorbonne Université CNRS‐INSU, Institut des Sciences de la Terre Paris, ISTeP Paris ,France
   Paris 1 Pantheon‐Sorbonne Université, CNRS‐Ministère de la Culture, Archéologies et Sciences de l'Antiquité, ArScAn UMR 7041, F‐92023 Nanterre ,France
   Instituto de Ciencias del Mar, CSIC, 08003 Barcelona, Spain
   GéoazurUniversité de Nice‐ Sophia Antipolis CNRS‐OCA, France
   Dpto. de Geodinamica, Universidad de Granada Granada ,Spain
   Instituto Andaluz de Ciencias de la Tierra (CSIC‐UGR), Granada ,Spain
   Instituto Español de Oceanografía (IEO), C.O. Málaga, 29640 Fuengirola Málaga, Spain
   Université Mohammed V‐Agdal Rabat, Morocco
C2 UNIV SORBONNE, FRANCE
   UNIV SORBONNE, FRANCE
   CSIC, SPAIN
   UNIV NICE, FRANCE
   UNIV GRANADA, SPAIN
   CSIC, SPAIN
   IEO, SPAIN
   UNIV RABAT, MOROCCO
IF 4.851
TC 18
UR https://archimer.ifremer.fr/doc/00612/72436/71382.pdf
LA English
DT Article
CR MARLBORO
   SARAS
BO Côtes De La Manche
   Ramon Margalef
AB Since the Miocene, the thinned continental crust below the Alboran Sea as well as its overlying sedimentary cover have been undergoing deformation caused by both convergence of Eurasia and Africa and by deep processes related to the Tethyan slab retreat. Part of this deformation is recorded at the Xauen and Tofiño banks in the southern Alboran Sea. Using swath bathymetry and multichannel seismic reflection data, we identified different stages and styles of deformation. The South Alboran Basin is made up of Early Miocene to Pliocene sedimentary layers that correlate with the West Alboran Basin depocenter and are dominated by E‐W trending folds and thrusts. The Xauen and Tofiño Banks first recorded the phase of extension and strike‐slip movement during the slab retreat, followed by the phase of compressional inversion since the Tortonian and are now structured by tight folds, thrusts and mud bodies. This study proposes that the Banks were located on the southern inherited Subduction Tear Edge Propagator (STEP) fault related to the westward migration of the Alboran domain during the Miocene. The STEP fault zone, acting as a boundary between the African block and the Alboran block, was located along the onshore Jebha‐Nekor fault and the offshore Alboran Ridge and the Yusuf fault zone. Thick‐skinned and thin‐skinned shortening occurred when slab retreat stopped, and inversion began. The present‐day style of the deformation seems to be linked to a decollement level made of undercompacted shale on top of the Ghomaride complex. Key Points The reactivation of the Subduction Tear Edge Propagator fault zone on the southern edge of the Alboran Domain, forms the South Alboran Ridge The style of the present‐day structure of the South Alboran region implies an interaction between thick‐skinned and thin‐skinned tectonics Undercompacted shales and inherited crustal structures are involved in the structural evolution of the South Alboran Basin Accepted Articles Accepted, unedited articles published online and citable. The final edited and typeset version of record will appear in the future. e2019TC005885 Related Information Metrics Details This article is protected by copyright. All rights reserved. Publication History Accepted manuscript online: 06 March 2020 Manuscript accepted: 25 February 2020 Manuscript revised: 24 February 2020 Manuscript received: 15 September 2019 
PY 2020
PD MAR
SO Tectonics
SN 0278-7407
PU American Geophysical Union (AGU)
VL 39
IS 3
UT 000530645700016
DI 10.1029/2019TC005885
ID 72436
ER

EF