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Quaternary evolution of a large alluvial fan in a periglacial setting (Crau Plain, SE France) constrained by terrestrial cosmogenic nuclide (Be-10) ArchiMer
Molliex, Stephane; Siame, Lionel L.; Bourles, Didier L.; Bellier, Olivier; Braucher, Regis; Clauzon, Georges.
Located in the foreland of the Western Alps, the Crau Plain was the outlet of the Durance River in the Pleistocene. In order to constrain its geodynamic evolution in terms of chronology and denudation rates, the two main Quaternary deposits of this plain have been studied based on cosmogenic nuclide Be-10 concentration measurements along depth profiles. The abandonment of the Miramas and Luquier alluvial surfaces occurred at the beginning of glacial periods, Wurm (isotopic stage 4) and Riss (isotopic stage 6), respectively. Discrepancy in denudation rates under similar geomorphological and lithological conditions suggests different denudation processes during glacial and interglacial periods. The denudation rate has been estimated at about 25 mm ka(-1) for...
Tipo: Text Palavras-chave: Quaternary; Denudation rate; Cosmic ray exposure (CRE) dating; Be-10 depth profile; Provence; Periglacial setting.
Ano: 2013 URL: http://archimer.ifremer.fr/doc/00149/26040/24740.pdf
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The GROSMarin experiment: three dimensional crustal structure of the North Ligurian margin from refraction tomography and preliminary analysis of microseismic measurements ArchiMer
Dessa, Jean-xavier; Simon, Soazig; Lelievre, Marjorie; Beslier, Marie-odile; Deschamps, Anne; Bethoux, Nicole; Solarino, Stefano; Sage, Francoise; Eva, Elena; Ferretti, Gabriele; Bellier, Olivier; Eva, Claudio.
The deep structure of the North Ligurian margin and its contiguous Ligurian basin as well as the seismicity recorded in these zones are neither well understood nor precisely constrained. In order to better address these questions, there is a need for offshore instrumenting, which was realised for a duration of nearly 6 months during the GROSMarin (Grand Reseau d'Observation Sous-Marin) experiment. An array of 21 ocean bottom seismometers was deployed over the most active area of the margin and was complemented on land by mobile seismological stations that densified existing permanent networks. We also realised the acquisition of deep refraction seismic shots at sea in order to get a 3D distribution of velocities along the margin through travel time...
Tipo: Text Palavras-chave: North Ligurian margin; Ocean bottom seismometers; Refraction tomography; Velocity structure; Crustal units; Microseismicity.
Ano: 2011 URL: http://archimer.ifremer.fr/doc/00214/32544/31020.pdf
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