English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/161399
Share/Impact:
Statistics
logo share SHARE   Add this article to your Mendeley library MendeleyBASE
Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

Title

Salt Tectonics in the Atlas Mountains of Morocco

AuthorsVergés, Jaume ; Moragas, Mar ; Martín-Martín, J. D.; Saura, Eduard ; Casciello, Emilio ; Hunt, D.W.
KeywordsJurassic salt tectonics
Central High Atlas
Tazoult salt wall
Tazoult allochthonous salt body
Imilchil minibasins
Salt-influenced rifts
Jurassic Atlas basin
Issue Date2017
PublisherElsevier
CitationPermo-Triassic Salt Provinces of Europe, North Africa and the Atlantic Margins, Tectonics and Hydrocarbon Potential: 563-579 (2017)
AbstractThe principal objective of this paper is to summarize the large data set gathered in the last few years on the Early-Middle Jurassic diapiric evolution in the well-exposed Central High Atlas in Morocco. Field data on both structural geology and sedimentology of halokinetic sequences, significant remote sensing mapping using good quality satellite images, thermal modeling and subsidence analysis, balanced and restored cross sections, and analog modeling allowed us to construct an integrated tectono-sedimentary interpretation of a salt-related rift basin. Three characteristic regions are summarized here to show the tectonic and diapiric evolution of the study region: Tazoult, Azourki, and Imilchil. Salt ridges (Tazoult, Jbel Azourki, and Tassent salt walls) above blind basement faults developed a polygonal array bounding thick synclines (minibasins) with different orientations. The Imilchil minibasins show diachronous age of their infill, which is a typical characteristic of diapiric regions. The Tazoult and Jbel Azourki salt walls developed an allochthonous salt body starting during the Late Pliensbachian-Aalenian time. Although only Lower and Middle Jurassic halokinetic sedimentary sequences are preserved in most of the Central High Atlas, younger synclines (minibasins) along the northern boundary of the Atlas (Demnate region) show development of Late Jurassic and Early Cretaceous minibasins. At the larger scale, the diachronous evolution of the extension and diapirism along the Atlas Basin suggests that diapirism and salt withdrawal play an important role during the development of the High Atlas in Morocco, Saharan Atlas in Algeria, and Tunisian Atlas in a similar way as it is fabulously imaged across the onshore and offshore Atlantic Moroccan basins.
Publisher version (URL)https://doi.org/10.1016/B978-0-12-809417-4.00027-6
URIhttp://hdl.handle.net/10261/161399
ISBN978-0-12-811450-6
Appears in Collections:(Geo3Bcn) Libros y partes de libros
Files in This Item:
File Description SizeFormat 
accesoRestringido.pdf15,38 kBAdobe PDFThumbnail
View/Open
Show full item record
Review this work
 


WARNING: Items in Digital.CSIC are protected by copyright, with all rights reserved, unless otherwise indicated.