English   español  
Please use this identifier to cite or link to this item: http://hdl.handle.net/10261/181293
Share/Impact:
Statistics
logo share SHARE logo core CORE   Add this article to your Mendeley library MendeleyBASE

Visualizar otros formatos: MARC | Dublin Core | RDF | ORE | MODS | METS | DIDL
Exportar a otros formatos:

Title

The Ebro Deep-Sea Fan System

AuthorsNelson, C. Hans ; Maldonado, Andrés ; Coumes, Francis; Got, Henri; Monaco, Andre
Issue DateJun-1983
PublisherSpringer
CitationGeo-Marine Letters 3(2-4): 125-131 (1983)
AbstractThe Ebro Fan System consists of en echelon channel-levee complexes, 50×20 km in area and 200-m thick. A few strong reflectors in a generally transparent seismic facies identify the sand-rich channel floors and levee crests. Numerous continuous acoustic reflectors characterize overbank turbidites and hemipelagites that blanket abandoned channel-levee complexes. The interlobe areas between channel complexes fill with homogeneous mud and sand from mass flow and overbank deposition; these exhibit a transparent seismic character. The steep continental rise and sediment “drainage” of Valencia Trough at the end of the channel-levee complexes prevent the development of distributary channels and midfan lobe deposits
Description7 pages, 4 figures
Publisher version (URL)https://doi.org/10.1007/BF02462457
URIhttp://hdl.handle.net/10261/181293
Identifiersdoi: 10.1007/BF02462457
issn: 0276-0460
e-issn: 1432-1157
Appears in Collections:(ICTJA) Artículos
Files in This Item:
There are no files associated with this item.
Show full item record
Review this work
 


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