Menu
kabarpetang media

Construction Of The Pyreneo Languedocian Sedimentary Ridge And Associated Sediment

  • Share

Jallet L Giresse P. Construction of the pyreneolanguedocian sedimentary ridge and associated sediment waves in the deep western gulf of lions Western Mediterranean Mar.


Large Sediment Waves Over The Gulf Of Roses Upper Continental Slope Nw Mediterranean Sciencedirect

And Droz et al.

Construction of the pyreneo languedocian sedimentary ridge and associated sediment. Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. A maximum width of 200 km and a total length of 300 km The Pyreneo-Languedocian Sedimentary Ridge PLSR and the maximum thickness of the sedimentary series initially identified as the Catalan Fan by Got and Stanley deposited by the fan is about 3600 m Droz and Bellaiche 1974 or Pyrenean Canyon Deep Sedimentary Body 1985. Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean.

Jallet L Giresse P 2005 Construction of the Pyreneo-Languedocian sedimentary ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. On the other hand in spite of the essential role played by salt tectonics in generating the depocenter of the Pyreneo-Languedocian fan the fan lobate shape does not reflect the degree of saltsediment.

Construction of the Pyreneo-Languedocian sedimentary ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. Droz et al 2006 such as the Rhône deep-sea fan the Pyreneo-Languedocian submarine sedimentary complex and the. 1993 and fed by sediment funnelled in the converging network of the Pyreneo-Languedocian canyons.

Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. Mar Petrol Geol 2005 22. Mar Petrol Geol 22865888.

Proposed that the Pyreneo-Languedocian Ridge is an asymmetrical feature located on the right-hand side of the Sète Valley with strong similarities to the Var Ridge on the Provençal Margin Savoye et al. Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. This saltsediment interaction is clearly expressed in the present-day seafloor morphology by sedimentary ridges disposed parallel to tectonic lineaments.

Recent sedimentary events in the western Gulf of Lions Western Mediterranean. Flood R D Piper D J W Klaus A et al. Late Devonian glaciation.

Terrigenous sediment input resulted in the deposition of Plio-Quaternary siliciclastic deep-water systems the post-salt series having distinct thickness lateral extent and depositional architecture Reis et al 2005a. Quaternary turbidite systems on the northern margins of the Balearic Basin Western Mediterranean. 2001 proposed that the Pyreneo-Languedocian Ridge is an asymmetrical feature located on the right-hand side of the Sète Valley with strong similarities to the Var Ridge on the Provençal margin Savoye et al.

The late proterozoic glacial era. The architecture of the PL Ridge shows numerous similarities with the Var sedimentary Ridge Savoye et al 1993 in that it is characterized by the over-development of one levee the western one and by the occurrence of oblique asymmetrical sediment waves and continuous eastward migration of the valley Droz et al 1997. The late OrdovicianEarly Silurian glacial period.

Marine and Petroleum Geology 22 865888. The combined effect of Coriolis. Berné et al.

Development of migrating sediment waves during the construction of the Pyreneo-Languedocian Sedimentary Ridge The Ridge is a sedimentary body fed by several canyons and minor channels acting simultaneously even if the Creus Cape canyon has a leading role compared with the competing supply from the Sète Canyon. The PLSR is characterized by the presence of sediment waves which were initially interpreted as creep-folds Canals-. In deeper waters a thick sedimentary body named the Pyreneo-Languedocian Sedimentary Ridge PLSR.

Jallet L Giresse P. Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean. Late proterozoic rifting glacial sedimentation and sedimentary cycles in the light of windermere deposition Western Canada.

1993 and was fed by sediment funnelled in the converging network of the Pyreneo-Languedocian canyons. The Pyreneo-Languedocian Ridge In the western corner of the Gulf of Lions the Pyreneo-Languedocian Ridge is a 900-1000 m thick sediment accumulation at the. 1 was identified at the base of the continental slope by Berné and Loubrieu 1999 during the CALMAR cruise in 1997.

Because a sediment package deposited above salt tendstospreadinadirectionparalleltothemaxi-mum bathymetric slope a subcircular sedimentary. And Bellaiche 1985 and the PyreneoLanguedocian sedimentary ridge Berné et al 1999. 865 – 888 Article Download PDF View Record in Scopus Google Scholar.

Laurent Jallet Pierre Giresse Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean Marine and Petroleum Geology 101016jmarpetgeo200503008 22 6-7. The objective of this paper is to investigate the architecture of prodeltaicshoreface sediments deposited around the Last Glacial Maximum between 46 and 15calkyrBPattheshelfedgeandtoproposeascenario for sea-level oscillations during this. Article Google Scholar 3.

It is thus well-documented that part of the remaining sediment supply is bypassed and feeds the prograding continental slope Lofi et al 2003 the Rhône deep sea fan Droz and Bellaiche 1985 and the Pyreneo-Languedocian sedimentary ridge Berné et al 1999. 22 2005 pp. 1999 and Droz et al.

Laurent Jallet and Pierre Giresse Construction of the Pyreneo-Languedocian Sedimentary Ridge and associated sediment waves in the deep western Gulf of Lions Western Mediterranean Marine and Petroleum Geology 22 6-7 865 2005. Proc ODP Init Reports 1995 155.


A Uninterpreted And B Interpreted Dip Seismic Profile Am Med018 Download Scientific Diagram


Large Sediment Waves Over The Gulf Of Roses Upper Continental Slope Nw Mediterranean Sciencedirect


Large Sediment Waves Over The Gulf Of Roses Upper Continental Slope Nw Mediterranean Sciencedirect


Large Sediment Waves Over The Gulf Of Roses Upper Continental Slope Nw Mediterranean Sciencedirect


Large Sediment Waves Over The Gulf Of Roses Upper Continental Slope Nw Mediterranean Sciencedirect


Bathymetry Of The Western Mediterranean Contour Isolines 150 300 Download Scientific Diagram


Bathymetry Of The Western Mediterranean Contour Isolines 150 300 Download Scientific Diagram

  • Share

Leave a Reply

Your email address will not be published.