Éditeur(s) : HAL CCSD Wiley-Blackwell
Résumé : International audience
Dating the timing of motion on crustal shear zones is of tremendous importance for understanding the assembly of orogenic terranes. This objective is achieved in this paper by combining petrological and structural observations with novel developments in in situ U-Th-Pb geochronology of allanite. A greenschist facies shear zone within the Mont Blanc Massif is documented. Allanite is synkinematic and belongs to the mylonitic assemblage. LA-ICP-MS U-Th-Pb isotope analyses of allanite reveal high contents and highly radiogenic isotopic compositions of the common-Pb component. The use of measured Pb-isotope compositions of associated minerals (feldspars and chlorite) is critical for accurate common-Pb correction, and provides a powerful mechanism for linking allanite growth to the metamorphic assemblage. A mean 208Pb/232Th age of 29.44 ± 0.95 Ma is accordingly taken for synkinematic allanite crystallisation under greenschist facies conditions. This age reflects the timing of the Mont Blanc underthrusting below the Penninic Front and highlights the potential of directly dating deformation with allanite.
ISSN: 0954-4879

hal-00963545
https://hal.archives-ouvertes.fr/hal-00963545
DOI : 10.1111/ter.12066

Éditeur(s) : HAL CCSD Wiley
Résumé : International audience
In this paper, the generalized Stokes problem αu−νΔu+∇p=f, ∇u=0, is considered, where ν denotes the kinematic viscosity, α is a positive parameter proportional to the inverse of the time-step, and the source term f gathers the external forcing, the nonlinear term, and the explicit part of the linear term. The system is derived from a time discretization for the Navier-Stokes equation governing the motion of a two-dimensional incompressible fluid. A domain decomposition numerical method is developed for solving the system. The original domain is divided into several nonoverlapping subdomains, and in each subdomain the concerned equations are discretized by certain finite element methods. A new feature of the method is that the pressure p is required to be piecewise linear rather than piecewise constant, so that the nonphysical oscillations in the solution using piecewise linear pressure are eliminated. However, a difficulty in using piecewise linear pressure is that the Stokes problem in each subdomain involves Dirichlet boundary conditions on pressure at the interface, which is not a real Stokes problem. To avoid the difficulty, a modification is proposed which removes the continuity conditions on the pressure across the interface. In this way, the Stokes problem in each subdomain has only Dirichlet boundary conditions on the velocity. Formulations and discussions for both the methods are presented, which shows that the modified method is simpler than the original one. Numerical experiments are displayed to show the efficiency of the methods, especially that the modified method has the same accuracy as the original one.
ISSN: 0749-159X

hal-00730200
https://hal.archives-ouvertes.fr/hal-00730200

Éditeur(s) : HAL CCSD
Résumé : International audience
We propose using a distributed algorithm to count individuals in a population and to collect abiotic factors in order to characterize habitat. The first phase consists of detecting the presence of individuals from mapping ecotopes, the second allows counting the number of individuals and the last aggregates the numbers of individuals over several paths. We propose an approach that uses a wireless sensor network built on a linear architecture based on the concept of green tunnel. Here, each mote has a successor and a predecessor.
à venir

hal-00857694
https://hal.archives-ouvertes.fr/hal-00857694

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
P>The Strait of Hormuz area is a transition zone between the continental collision of the Zagros (west) and the subduction of an oceanic part of the Arabian Plate beneath the Makran wedge (east). Geology and recent GPS measurements indicate that about 15 mm yr-1 of relative motion in N10 degrees E direction is accommodated by two major fault systems: (1) the NNW-trending Minab-Zendan-Palami (MZP) fault system that connects the Main Zagros Thrust (MZT) to the inner Makran thrust system and the Frontal subduction thrust and (2) the N-trending Sabzevaran-Kahnuj-Jiroft (SKJ) fault system that bounds the Jazmurian depression to the west. We use dense GPS measurements along four transects across these fault systems in order to determine the strains spatial distribution. The northern GPS transect confirms the total fault slip rates for both fault systems estimated by the tectonic analyses (about 10 and 7.3 mm yr-1 in N10 degrees direction across the MZP and SKJ fault systems, respectively). For both fault systems, the elastic deformation spreads over shear zones that are several tens of kilometres wide. However, transects located close to latitude 27 degrees N reveal a much narrower shear zone (similar to 10 km) for the MZP fault system. Moreover, we confirm that most of the present-day strain is transferred towards the frontal subduction thrust rather than towards the inner Makran thrusts. In order to complement this new GPS velocity field with spatially dense measurements, we processed a set of ERS radar images by the radar interferometry (InSAR) technique. We used both a 'stacking' and a 'persistant-scatterers' approach to differentiate the ground deformation signal which spatial gradient is expected to be very low, from the atmospheric signal. Results from these interferograms appear to be relatively in agreement with the GPS-determined strain distribution. Nevertheless, they confirm the absence of any superficial creep behaviour since no sharp discontinuity on interferometric phase can be noted on any interferogram. Finally, we use a purely kinematic 'block model' inversion process to calculate slip rates and locking depths for each fault system from our GPS measurements. These models suggest that the relative quiescence over the last 200 yr has certainly produced a slip deficit as high as 2 m. So, we may wonder if the MZP fault system is not late in the interseismic phase of its earthquake cycle.
ISSN: 0956-540X

hal-00429386
https://hal.archives-ouvertes.fr/hal-00429386
DOI : 10.1111/j.1365-246X.2009.04321.x

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Recent global kinematic studies reveal that most of the trenches roll back but a significant number of them advance toward the upper plate. Those advancing trenches are mostly located in the Western Pacific and correspond to the subduction of very old, Mesozoic oceanic lithosphere. While retreating trenches are commonly explained by the slab pull action of the descending lithosphere, the origin of advancing trenches is still debated. Since this relationship is dependent upon the adopted reference frame, we select region where geological studies show the variability of trench migration style with time. The Izu-Bonin-Mariana (IBM) region represents a key example. The detailed reconstruction of the trench migration of the IBM subducting system reveals that after a long episode of asymmetric rollback, the IBM trench recently started advancing. We propose that this change from retreating to advancing trench mode results from the subduction of progressively older and stiffer lithospheric material. We test this hypothesis by means of two-dimensional (2-D) numerical models, reproducing the effects of the lithospheric aging during subduction. The result of our numerical tests shows that the entrance of old and stiff lithosphere forces the trench to advance because the increasing stiffness of the slab prevents the slab to unbend once it has subducted. We adapt this physical result to the IBM evolution, showing that the switch from trench retreat to trench advance can reconcile the shape of IBM slab as previously suggested. Finally we discuss the possibility that the subduction of the Cretaceous lithosphere might have triggered the change of the motion of the Pacific plate around 5 Ma.
ISSN: 0012-821X

hal-00455988
https://hal.archives-ouvertes.fr/hal-00455988
DOI : 10.1016/j.epsl.2009.09.042

Éditeur(s) : HAL CCSD
Résumé : International audience
The environmental uncertainty leads SMEs to adopt collective strategies in order to supplement their inadequate resources. The longitudinal study of the Pic Saint-Loup union of wine producers provides an understanding of how SMEs can develop collective strategies. The case study is based on several time of data collection from mainly forty five semi-structured interviews. Our findings are twofold. We identify the stages of SMEs collective strategies development and the role of stakeholders. Then, we highlight the tertius strategies of SMEs owner-managers and the positive influence of their combination.
Les PME, plus vulnérables aux forces de l'environnement, cherchent à compléter l'insuffisance de leurs ressources en adoptant des stratégies collectives afin de réduire cette incertitude. L'étude longitudinale du syndicat de producteurs de vin du Pic Saint-Loup, qui s'appuie sur plusieurs temps de collecte et quarante-cinq entretiens semi-directifs, permet de comprendre la façon dont des PME peuvent développer des stratégies collectives. Nous identifions les phases du développement de la stratégie collective ainsi que le rôle joué par les parties prenantes. Puis, nous soulignons les stratégies de tertius des dirigeants de PME et leur combinaison favorisant le développement de ces stratégies collectives. Mots clés : Stratégie collective, PME, étude longitudinale, parties prenantes, tertius. *Remerciements Ce papier bénéficie du soutien de la chaire Entrepreneuriat et Innovation du 'Labex Entreprendre' de Montpellier en France. Ce " laboratoire d'excellence " est reconnu et soutenu par le gouvernement français pour la qualité de ses recherches dans les sciences humaines et sociales.
Management International / International Management / Gestión Internacional

hal-01588177
http://hal.univ-smb.fr/hal-01588177
http://hal.univ-smb.fr/hal-01588177/document
http://hal.univ-smb.fr/hal-01588177/file/MI-710%20-%20GRANATA%20DA%20FONSECA%20MARQU%C3%88S%20G%C3%89RAUDEL.pdf

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We present Contact Dynamics discrete element simulations of the earthquake-triggered Jiufengershan avalanche, which mobilized a 60 m thick, 1.5 km long sedimentary layer, dipping similar to 22 degrees SE toward a valley. The dynamic behavior of the avalanche is simulated under different assumptions about rock behavior, water table height, and boundary shear strength. Additionally, seismic shaking is introduced using strong motion records from nearby stations. We assume that seismic shaking generates shearing and frictional heating along the surface of rupture, which, in turn, may induce dynamic weakening and avalanche triggering; a simple "slip-weakening'' criterion was adopted to simulate shear strength drop along the rupture surface. We investigate the mechanical processes occurring during triggering and propagation of an avalanche mobilizing shallowly dipping layers. Incipient deformation forms a pop-up structure at the toe of the dip slope. As the avalanche propagates, the pop-up deforms into an overturned fold, which overrides the surface of separation along a decollement. Simultaneously, uphill layers slide at high velocity (125 km/h) and are folded and disrupted as they reach the toe of the dip slope. The avalanche foot forms a wedge that is pushed forward as deformed rocks accrete at its rear. We simulated five cross sections across the Jiufengershan avalanche, which differ in the geometry of the surface of separation. Topographic and simulated surface profiles are similar. The friction coefficient at the surface of separation determined from back analysis is abnormally low (mu(SS) = 0.2), possibly due to lubrication by liquefied soils. The granular deposits of simulated earthquake- and rain-triggered avalanches are similar.
ISSN: 0148-0227

hal-00420882
https://hal.archives-ouvertes.fr/hal-00420882
DOI : 10.1029/2008JF001075

Éditeur(s) : HAL CCSD
Résumé : Report
This activity uses available information on vertical land motion and on global glacier and ice sheet mass balance to make projections of sea-level change (to the year 2100) for Arctic communities and vital infrastructure.
https://hal.archives-ouvertes.fr/hal-00856635

hal-00856635
https://hal.archives-ouvertes.fr/hal-00856635

Résumé : La tribologie est définie comme la science qui étudie les phénomènes de frottement, d’usure et de lubrification. Elle intervient à chaque fois que deux surfaces sont en mouvement relatif l’une par rapport à l’autre. On la rencontre donc principalement dans les moteurs, les instruments de coupe, les assemblages mécaniques etc. Le frottement et l’usure sont les causes principales des pertes de performances et de durabilité des systèmes. L’usure coute 3 % du PIB en France et on estime que 10 % à 30 % de l’énergie produite dans le monde est consommée par frottement, c’est dire l’importance que porte le monde industriel à cette science.C'est la lubrification qui a pour rôle de minimiser le frottement et de protéger les surfaces de l'usure. Il existe différents régimes de lubrification, cependant les travaux effectués au cours de cette thèse de doctorat s’intéressent exclusivement au régime de lubrification limite. Dans ce régime de lubrification, l’épaisseur du film de lubrifiant est du même ordre de grandeur que la hauteur des aspérités des surfaces en contact et le frottement et l'usure des surfaces peuvent être très sévères. La stratégie mise en place pour lutter contre ces phénomènes consiste à ajouter des additifs à l'huile lubrifiante, qui formeront au cours du frottement un film protecteur (le tribofilm). Il apparait donc primordial de bien caractériser ces tribofilms afin de mieux comprendre les mécanismes de réduction de frottement et de l’usure, qui restent encore à ce jour mal connus.Les nanotechnologies permettent aujourd'hui d'apporter un nouvel éclairage sur cette problématique et nous les avons mises à profit pour étudier le comportement mécanique des tribofilms à l’échelle nanométrique.L’objectif de ce travail est de comprendre les processus de réduction de frottement observés à l’échelle macroscopique lorsque des particules de composés lamellaires sont associées à un liquide de faible viscosité. Les tribofilms étudiés sont formés à partir de trois composés lamellaires différents, le graphite, le thiophosphate de nickel NiPS3 et le bisulfure de molybdène MoS2. Pour ces trois composés, deux types de tribofilms ont été étudiés : ceux formés à partir des particules seules (les tribofilms secs) et ceux formés en présence de liquide (les tribofilms éther).L’analyse des propriétés tribologiques mesurées à macro et nano échelle, nous ont permis de mieux comprendre la contribution des effets individuels et collectifs sur les mécanismes réducteurs de frottement. Ces expériences ont permis de mettre en évidence que la réduction du coefficient de frottement observée à macro-échelle n'est pas due à la nanostructuration des tribofilms ni à une baisse des interactions entre les feuillets mais plutôt à un effet collectif des particules et du liquide.
Tribology is the science of friction phenomena, wear and lubrication. It takes part every time two surfaces are in relative motion. It performs meanly in engine and mechanical systems. Friction and wear are the mean reasons of loose of performance and durability of mechanical systems. Wear costs 3% of the GDP in France and about 10% to 30% of the produced energy in the world is consumed by friction.The aim of lubrication is to reduce friction and protect the surface against wear. There are four different types of lubrication regimes but this study is focused on the boundary regime. In this regime, lubricant thickness is of the same order of the magnitude of the sliding surfaces roughness, leading to a high-level of friction and wear. Additives are added to the lubricating base oil, in order to build a protecting tribofilm. Characterization of the tribofilms appears essential to better understand the friction and wear reduction mechanisms.Nanotechnology allows to bring a new insight on this issue through the study of the mechanical behavior of the tribofilms at nanoscale.The aim of this work is to better understand the process of the friction reduction observed at macroscale when lamellar particles are associated to a low viscosity liquid. The tribofilms are formed from three different lamellar compounds, graphite, nickel thiophosphate NiPS3 and molybdenum disulfide MoS2. Two different kinds of tribofilms are studied: those formed with the solids particles only (dry tribofilms) and those formed in presence of liquid (wet tribofilms).The analyses of the tribological properties measured at nanoscale allow us to better understand the contribution of the individual and collective effects on friction reduction mechanims. We show that the reduction of the friction coefficient observed at macroscale is not related to the surface nanostructuration of the tribofilms neither to the decrease of the interaction energy between the sliding surfaces, but rather to collective effects of the liquid and the particles in the contact.

http://www.theses.fr/2014AGUY0706/document

Éditeur(s) : HAL CCSD
Résumé : International audience
This work presents a synthesis of the present-day knowledge on both emerged and submerged carbonate platforms of the Guadeloupe archipelago. Onshore and offshore data acquired during the KaShallow project are presented. Since the early Zanclean, some isolated platforms developed onto a Jurassic to Tortonian basement which displayed reliefs inherited from a major extensional tectonic episode dated from −8 to −5 Ma. Marie-Galante, Grande Terre and the southern shelf of Grande-Terre show strong similarities with Zanclean to Gelasian red-algal facies upward changing into early Calabrian coral facies. A major erosional unconformity (SB2) was recognized and allows to distinguish two early Calabrian formations (Calcaires à Agaricia Formation and Calcaires à Acropora Formation). The final emersion of these platforms is late Calabrian. The La Désirade platform displays Zanclean to early Piacenzian red-algal facies upward changing into coral facies. This platform emerged as soon as in the late Piacenzian. The island subsided again in relation with later extensional tectonic episode and early Calabrian reef platform then unconformably deposited. The Colombie bank deposits comprise Pliocene basinal deposits overlain by late Calabrian coral reefs. The Flandre bank might have emerged synchronously with La Désirade but was drowned only in the late Pleistocene-Holocene interval. Four extensional tectonic episodes have been identified in the late Miocene-Recent interval. Their effects depend on the location of the platforms within the fore-arc.
Bulletin Société Géologique de France

insu-00816463
https://hal-insu.archives-ouvertes.fr/insu-00816463
DOI : 10.2113/gssgfbull.184.1-2.99

Éditeur(s) : HAL CCSD
Résumé : International audience
We propose using a distributed algorithm to count individuals in a population by way of a 3-phase algorithm. The first phase consists of detecting the presence of individuals, the second allows counting the number of individuals and the last aggregates the numbers of individuals over several paths. We propose an approach that uses a wireless sensor network built on a linear architecture. Here, each mote has a successor and a predecessor.
Wireless Communications in Unusual and Confined Areas (ICWCUCA), 2012 International Conference on

hal-00857695
https://hal.archives-ouvertes.fr/hal-00857695
DOI : 10.1109/ICWCUCA.2012.6402496

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
In the Gulf of Cadiz key segment of the Africa-Iberia plate boundary (North-East Atlantic ocean), three main different modes of tectonic interference between a recently identified wrench system (SWIM) and the Gulf of Cadiz Accretionary Wedge (GCAW) were tested through analog sand-box modeling: a) An active accretionary wedge on top of a pre-existent inactive basement fault; b) An active strike-slip fault cutting a previously formed, inactive, accretionary wedge; and c) Simultaneous activity of both the accretionary wedge and the strike-slip fault. The results we obtained and the comparison with the natural deformation pattern favor a tectonic evolution comprising two main steps: i) the formation of the Gulf of Cadiz Accretionary Wedge on top of inactive, Tethyan-related, basement faults (Middle Miocene to ~ 1.8 Ma); ii) subsequent reactivation of these basement faults with dextral strike-slip motion (~ 1.8 Ma to present) simultaneously with continued tectonic accretion in the GCAW. These results exclude the possibility of ongoing active SWIM wrench system cross-cutting an inactive GCAW structure. Our results also support a new interpretation of the SWIM wrench system as fundamentally resulting from strike-slip reactivation of an old (Tethyan-related) plate boundary.
ISSN: 0025-3227

insu-00643630
https://hal-insu.archives-ouvertes.fr/insu-00643630
https://hal-insu.archives-ouvertes.fr/insu-00643630/document
https://hal-insu.archives-ouvertes.fr/insu-00643630/file/Duarte_etal_2011_MS-1.pdf
DOI : 10.1016/j.margeo.2011.09.014

Éditeur(s) : HAL CCSD
Résumé : International audience
Nous avons tous déjà eu l'occasion d'effectuer des recherches d'ordre médical sur Internet. Si certains sites spécialisés se refusent à tout diagnostic en ligne, préférant le renvoi vers des professionnels de santé, d'autres en revanche conduisent souvent à des déclarations alarmistes faisant état de situations humaines difficiles. Dans ce travail, nous étudions l'ampleur de ce phénomène et montrons que quel que soit le syndrome recherché, les résultats obtenus conduisent toujours à l'énoncé des mots" cancer" ou" tumeur".
Extraction et gestion des connaissances
Rennes, France

hal-01312315
https://hal.archives-ouvertes.fr/hal-01312315

Éditeur(s) : Paris : Grassart
Siècle(s) traité(s) : 19
Droits : Domaine public
Provenance : Archives territoriales de Guyane
Permalien : http://www.manioc.org/patrimon/GAD11056
GAD11056

Éditeur(s) : Paris : Lecointe et Durey
Siècle(s) traité(s) : 15
Droits : Domaine public
Provenance : Conseil départemental de la Guadeloupe. La Médiathèque Caraïbe
Permalien : http://www.manioc.org/patrimon/LAM17007
LAM17007