Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
New evolutionary models for the Pyrenean orogeny must consider feedbacks between the Mid-Cretaceous hyperextension postulated recently and the Pyrenean inversion. We present a new crustal section of the Pyrenees through the Jaca Basin, the western Axial Zone and the Chaînons Béarnais, which allows identifying the ancient continental margins of the Iberian and European plates and a suture. A sequential restoration allows a reassessment of the style of convergence through time. Restoration leads to a progressively thinned crust in narrow continental margins separated by a domain of exhumed mantle peridotite and overlain by a detached sedimentary lid. Early convergence during the Late Cretaceous and the Earliest Paleogene was accommodated by subduction of the peridotite domain. This was followed in the Eocene by initial collision involving overriding of the Iberian margin onto the European margin along the deep ramp of the North-Pyrenean Frontal thrust, which defines the suture. Subsequent full collision and strong relief generation from the late-Mid or Late Eocene to the Early Miocene were associated with thrust accretion of the Iberian plate, underlain by wedging and northward subduction of the decoupled Iberian lower crust.
ISSN: 1631-0713

insu-01291223
https://hal-insu.archives-ouvertes.fr/insu-01291223
https://hal-insu.archives-ouvertes.fr/insu-01291223/document
https://hal-insu.archives-ouvertes.fr/insu-01291223/file/The%20crustal%20evolution%20of%20the%20west-central%20Pyrenees%20-%20postprint.pdf
DOI : 10.1016/j.crte.2015.10.010

Éditeur(s) : HAL CCSD
Résumé : Transposable elements play a major role in the evolution of eukaryotic genomes. Knowing the distribution of transposable elements between different species within the same taxon is essential to study their dynamics and to better understand their role in the evolution of species. Given their abundance, species diversity and living environment, crustaceans are an excellent model for studying comparative genomics of retrotransposons. It is notably in the squat lobsters that the GalEa clade of Superfamily Copia was defined. We studied the distribution of two well-known LTR retrotransposons superfamilies: Gypsy and Copia, in crustaceans. By combining PCRs with degenerate primers and in silico analysis, we identified 35 families of Copia retrotransposons and 46 families of Gypsy retrotransposons in 15 and 18 species of crustaceans (mainly Malacostraca: crabs, shrimp, krill ...). These elements have different distribution and diversity in crustaceans. Gypsy elements appear relatively commonly and diverse in all species. Conversely, the Copia elements seem rare, and consequently more difficult to detect, and are largely dominated by the elements of the clade GalEa. These results suggest two different dynamic strategies for retrotransposons Gypsy (the Red Queen theory) and retrotransposons GalEa (‘domino days spreading’ branching process). In addition, GalEa elements present a great evolutionary success being widely distributed in many branches of metazoans. They are also present in certain red algae and we have also detected them in Fungi. Taking advantage of the large amount of available genomic data, we have studied the distribution of GalEa elements of Fungi, in order to compare it with the results obtained in crustaceans. In fact, they appear only in a large phylum of Ascomycetes, in Pezizomycotina, and they form a monophyletic group within the GalEa. Finally, in the Fungi, the GalEa elements are not majority among Copia retrotransposons. We have therefore initiated a new study in molluscs, to define if the results obtained in crustaceans are a feature of GalEa elements, Malacostraca or metazoans.
Les éléments transposables jouent un rôle majeur dans l’évolution des génomes eucaryotes. La connaissance de la distribution des éléments transposables entre différentes espèces au sein d’un même taxon est une condition essentielle pour étudier leur dynamique et mieux comprendre leur rôle dans l'évolution des espèces. Compte tenu de leur abondance, de leur diversité spécifique et de milieu de vie, les crustacés sont un excellent modèle pour étudier la génomique comparative des rétrotransposons. C’est notamment chez les Galathées qu’a été défini le clade GalEa des éléments de la superfamille des Copia. Nous avons étudié la distribution de deux superfamilles de rétrotransposons à LTR bien connus: les Gypsy et les Copia, au sein des crustacés. En combinant des PCRs avec amorces dégénérées et des analyses in silico, nous avons identifié 35 familles de rétrotransposons Copia et 46 familles de rétrotransposons Gypsy dans respectivement 15 et 18 espèces de crustacés (principalement des malacostracés : crabes, crevettes, krill...). Ces éléments présentent une distribution et une diversité différentes au sein des crustacés. Les éléments Gypsy apparaissent relativement fréquents et diversifiés dans toutes les espèces. A l’inverse, les éléments Copia semblent rares, donc difficilement détectables, et sont largement dominés par les éléments du clade GalEa. Ces résultats suggèrent deux stratégies différentes de dynamique pour les rétrotransposons Gypsy (théorie de la Reine Rouge) et les rétrotransposons GalEa (‘domino days spreading’ branching process). De plus, les éléments GalEa présentent un grand succès évolutif en étant largement distribués dans de nombreuses branches de métazoaires. Ils sont aussi présents chez quelques algues rouges et nous en avons également détecté chez des Fungi. Profitant des nombreuses données génomiques disponibles, nous avons donc étudié la distribution des éléments GalEa de Fungi, dans le but de comparer celle-ci aux résultats obtenus chez les crustacés. En fait, ils n’apparaissent qu’au sein d’un grand embranchement d’ascomycètes, les Pezizomycotina, et ils forment un groupe monophylétique au sein des GalEa. Enfin, chez les Fungi, les éléments GalEa ne sont pas majoritaire parmi les rétrotransposons Copia. Nous avons donc initié une nouvelle étude chez les mollusques, afin de définir si les résultats obtenus chez les crustacés sont une caractéristique des éléments GalEa, des malacostracés ou des métazoaires.
https://tel.archives-ouvertes.fr/tel-01132413

NNT : 2015PA066017
tel-01132413
https://tel.archives-ouvertes.fr/tel-01132413
https://tel.archives-ouvertes.fr/tel-01132413/document
https://tel.archives-ouvertes.fr/tel-01132413/file/these_archivage_2600252o.pdf

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
We use 3 yr of surface absolute gravity measurements at three sites on the Larzac plateau (France) to quantify the changes induced by topography and the building on gravity time-series, with respect to an idealized infinite slab approximation. Indeed, local topography and buildings housing ground-based gravity measurement have an effect on the distribution of water storage changes, therefore affecting the associated gravity signal. We first calculate the effects of surrounding topography and building dimensions on the gravity attraction for a uniform layer of water. We show that a gravimetric interpretation of water storage change using an infinite slab, the so-called Bouguer approximation, is generally not suitable. We propose to split the time varying gravity signal in two parts (1) a surface component including topographic and building effects (2) a deep component associated to underground water transfer. A reservoir modelling scheme is herein presented to remove the local site effects and to invert for the effective hydrological properties of the unsaturated zone. We show that effective time constants associated to water transfer vary greatly from site to site. We propose that our modelling scheme can be used to correct for the local site effects on gravity at any site presenting a departure from a flat topography. Depending on sites, the corrected signal can exceed measured values by 5-15 μGal, corresponding to 120-380 mm of water using the Bouguer slab formula. Our approach only requires the knowledge of daily precipitation corrected for evapotranspiration. Therefore, it can be a useful tool to correct any kind of gravimetric time-series data.
ISSN: 0956-540X

hal-00795590
https://hal.archives-ouvertes.fr/hal-00795590
DOI : 10.1093/gji/ggs007

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
An exploration 3D seismic data set from the Gjallar Ridge off mid-Norway images a giant fluid seep structure 3 × 5 km wide, which connects to late Palaeocene magmatic sills at depth. Two of the pipes that have developed as hydrothermal vents reach all the way to the modern seafloor implying that they either were active much longer than the original hydrothermal activity or have been reactivated. We combine detailed seismic analysis of the northern pipe and sandbox modeling to constrain pipe initiation and propagation. Although both the seismic data and the sandbox models suggest that fluids at depth are focused through a vertical conduit, sandbox models show that fluids ascend and reach a critical depth migration where focused migration abruptly transforms into distributed fluid flow through unconsolidated sediments. This indicates that at this level the sediments are intensely deformed during pipe propagation, creating a V-shaped structure, i.e. an inverted cone at depth and a positive relief anomaly, 5 to 10 m high, at the seafloor, which is clearly identified on 3D seismic data. Comparison of the geometries observed in sandbox modeling with the seismically observed geometries of the Giant Gjallar Vent suggests that the Giant Gjallar Vent may be a proto-fluid seep at an early stage of its development, preceding the future collapse of the structure forming a seafloor depression. Our results imply that the Gjallar Giant Vent can be used as a window into the geological processes active in the deep parts of the Vøring Basin.
ISSN: 0025-3227

hal-00772465
https://hal.archives-ouvertes.fr/hal-00772465
DOI : 10.1016/j.margeo.2012.08.010

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We report measurements of long-period P wave polarization (P pol) in Australia and Tahiti made by combining modeling of the polarization deviation and harmonic analysis. The analysis of the deviation of the horizontal polarization of the P wave as a function of event back azimuth may be used to obtain information about (1) sensor misorientation, (2) dipping discontinuities, (3) seismic anisotropy, and (4) velocity heterogeneities beneath a seismic station. The results from harmonic analysis and a grid search using Snell's law suggest the presence of a dipping seismic discontinuity beneath stations CTAO and CAN in Australia. These results are consistent with published receiver function studies for these stations. The P pol fast axis orientation is close to the N–S absolute plate motion direction at station TAU (Tasmania), which may be due to plate-motion-driven alignment of olivine crystals in the asthenosphere. Interestingly, measurements of SKS splitting at Tahiti (French Polynesia) show an apparent isotropy, whereas an inversion of P pol observations at PPTL seismic station located in Tahiti suggests the presence of two anisotropic layers. The fast axis azimuth is oriented E–W in the upper layer, and it is close to the NW–SE orientation in the lower layer. Since P pol orientations are used for real-time earthquake locations, especially in poorly instrumented areas such as the South Pacific, we show that the bias from anisotropy and sensor misorientation determined here can be corrected to improve the location accuracy, which yields fundamental data for rapid location necessary for effective tsunami warning.
ISSN: 2169-9313

hal-01389113
http://hal.univ-reunion.fr/hal-01389113
http://hal.univ-reunion.fr/hal-01389113/document
http://hal.univ-reunion.fr/hal-01389113/file/Fontaine_Ppol_JGR2009.pdf
DOI : 10.1029/2008JB005709

Éditeur(s) : HAL CCSD
Résumé : Patagonia is well known for spectacular occurrences of a variety of glacial-derived landforms and deposits and for a long history of ancient glaciations. In this paper, we first review the diverse evidence that demonstrates the development of glacial-related sedimentary units within the Central Patagonian Cordillera since 7 Ma. Well preserved glacial landforrns at the top surface of mesetas on both sides of the Lago General Carrera-Buenos Aires are described: the Meseta Guenguel to the north, and the volcanic Meseta del Lago Buenos Aires to the south. The latter meseta corresponds to a 3 Ma old, morphologically inverted paleo-piedmont, based on Ar/Ar dates of the uppermost lava flows. It shows evidence of glacier advances to the NE direction. Over a distance of 20 km, glacial landforms observed by remote sensing data and digital elevation model define glacial tongues that were fed by the Cordillera reliefs to the west. These lobes are now beheaded from their westward sources along a morpho-structural corridor that bounds the Meseta del Lago Buenos Aires to the west. These remnants can be correlated with the oldest glacial landforms recognized north of Lago General Carrera-Buenos Aires, on the Meseta Guenguel that form the Chipanque moraine system. From these features it is concluded that the glacial drainage network of Central Patagonia has been strongly modified following relief inversion in response to erosion processes and to tectonic causes. Changes occurred after 3 Ma, from a smooth piedmont surface covered by an extensive ice mantle ending with ample glacial lobes, to the current series of deeply incised glacial valleys such as the Lago General Carrera-Buenos Aires depression. These new data bear important constraints on the history and development of the first glaciations in southern South America.
ANDEAN GEOLOGY

hal-00512682
https://hal.archives-ouvertes.fr/hal-00512682

Éditeur(s) : Wiley / Blackwell
Résumé : For the first time, a deep seismic data set acquired in the frame of the Algerian-French SPIRAL program provides new insights regarding the origin of the westernmost Algerian margin and basin. We performed a tomographic inversion of traveltimes along a 100-km-long wide-angle seismic profile shot over 40 ocean bottom seismometers offshore Mostaganem (Northwestern Algeria). The resulting velocity model and multichannel seismic reflection profiles show a thin (3-4 km thick) oceanic crust. The narrow ocean-continent transition (less than 10 km wide) is bounded by vertical faults and surmounted by a narrow almost continuous basin filled with Miocene to Quaternary sediments. This fault system, as well as the faults organized in a negative-flower structure on the continent side, marks a major strike-slip fault system. The extremely sharp variation of the Moho depth (up to 45 +/- 3 degrees) beneath the continental border underscores the absence of continental extension in this area. All these features support the hypothesis that this part of the margin from Oran to Tenes, trending N65-N70 degrees E, is a fossil subduction-transform edge propagator fault, vestige of the propagation of the edge of the Gibraltar subduction zone during the westward migration of the Alboran domain.
Geophysical Journal International (0956-540X) (Wiley / Blackwell), 2015-02 , Vol. 200 , N. 2 , P. 1027-1043

Droits : The Authors 2014. Published by Oxford University Press on behalf of The Royal Astronomical Society
http://archimer.ifremer.fr/doc/00255/36670/35278.pdf
http://archimer.ifremer.fr/doc/00255/36670/35279.pdf
DOI:10.1093/gji/ggu454
http://archimer.ifremer.fr/doc/00255/36670/

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
BACKGROUND: HIV cohort collaborations, which pool data from diverse patient cohorts, have provided key insights into outcomes of antiretroviral therapy (ART). However, the extent of, and reasons for, between-cohort heterogeneity in rates of AIDS and mortality are unclear. METHODS: We obtained data on adult HIV-positive patients who started ART from 1998 without a previous AIDS diagnosis from 17 cohorts in North America and Europe. Patients were followed up from 1 month to 2 years after starting ART. We examined between-cohort heterogeneity in crude and adjusted (age, sex, HIV transmission risk, year, CD4 count and HIV-1 RNA at start of ART) rates of AIDS and mortality using random-effects meta-analysis and meta-regression. RESULTS: During 61 520 person-years, 754/38 706 (1.9%) patients died and 1890 (4.9%) progressed to AIDS. Between-cohort variance in mortality rates was reduced from 0.84 to 0.24 (0.73 to 0.28 for AIDS rates) after adjustment for patient characteristics. Adjusted mortality rates were inversely associated with cohorts' estimated completeness of death ascertainment [excellent: 96-100%, good: 90-95%, average: 75-89%; mortality rate ratio 0.66 (95% confidence interval 0.46-0.94) per category]. Mortality rate ratios comparing Europe with North America were 0.42 (0.31-0.57) before and 0.47 (0.30-0.73) after adjusting for completeness of ascertainment. CONCLUSIONS: Heterogeneity between settings in outcomes of HIV treatment has implications for collaborative analyses, policy and clinical care. Estimated mortality rates may require adjustment for completeness of ascertainment. Higher mortality rate in North American, compared with European, cohorts was not fully explained by completeness of ascertainment and may be because of the inclusion of more socially marginalized patients with higher mortality risk.
ISSN: 0300-5771

hal-00875138
https://hal.archives-ouvertes.fr/hal-00875138
DOI : 10.1093/ije/dys164
PUBMED : 23148105

Éditeur(s) : HAL CCSD Royal Society
Résumé : International audience
The 2 465 177 bp genome of Sulfolobus islandicus LAL14/1, host of the model rudivirus SIRV2, was sequenced. Exhaustive comparative genomic analysis of S. islandicus LAL14/1 and the nine other completely sequenced S. islandicus strains isolated from Iceland, Russia and USA revealed a highly syntenic common core genome of approximately 2 Mb and a long hyperplastic region containing most of the strain-specific genes. In LAL14/1, the latter region is enriched in insertion sequences, CRISPR (clustered regularly interspaced short palindromic repeats), glycosyl transferase genes, toxin-antitoxin genes and MITE (miniature inverted-repeat transposable elements). The tRNA genes of LAL14/1 are preferential targets for the integration of mobile elements but clusters of atypical genes (CAG) are also integrated elsewhere in the genome. LAL14/1 carries five CRISPR loci with 10 per cent of spacers matching perfectly or imperfectly the genomes of archaeal viruses and plasmids found in the Icelandic hot springs. Strikingly, the CRISPR_2 region of LAL14/1 carries an unusually long 1.9 kb spacer interspersed between two repeat regions and displays a high similarity to pING1-like conjugative plasmids. Finally, we have developed a genetic system for S. islandicus LAL14/1 and created ΔpyrEF and ΔCRISPR_1 mutants using double cross-over and pop-in/pop-out approaches, respectively. Thus, LAL14/1 is a promising model to study virus-host interactions and the CRISPR/Cas defence mechanism in Archaea.
ISSN: 2046-6390

hal-00818894
https://hal.archives-ouvertes.fr/hal-00818894
DOI : 10.1098/rsob.130010
PUBMED : 23594878

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Crystal growth driven by a flowing solution is modeled for a flow with low Reynolds number using a computational dynamic software. Considering equivalent crystallographic faces, the chemical flux is calculated along upstream and downstream faces. Upstream flux is higher compared to downstream and leads to a symmetry breakdown of the crystal shape and develops mirror symmetry parallel to the flow velocity. Moreover the ratio of these two fluxes (upstream / downstream) gives a quantitative relation between the relative crystal growth rate and the flow velocity. Thus, using an inverse method, the flow direction and velocity can be deduced by the study of the variation of the growth band thicknesses of equivalent crystallographic faces. This new method was applied to the formation of metasomatic tourmalinite associated with a leucogranite sill. The approach is complemented by a study of the chemistry of the tourmaline. In the studied case, the application of the new method gives the high fluid velocities in pores (10-3 - 10-4 m/s) during metasomatism. Equivalent Darcy velocities are estimated and discussed accounting for the major role played by the regional deformation. Finally, a two-stage tectono-hydrodynamic model is proposed for the metsomatism. The first stage is genetically linked to the sill injection, and the second is characterized by a wider event with hydrothermal flow passing along the leucogranite sills.
ISSN: 0012-821X

Droits : info:eu-repo/semantics/OpenAccess
insu-00352307
https://hal-insu.archives-ouvertes.fr/insu-00352307
https://hal-insu.archives-ouvertes.fr/insu-00352307/document
https://hal-insu.archives-ouvertes.fr/insu-00352307/file/Sizaret_et_al_final.pdf
DOI : 10.1016/j.epsl.2009.01.013

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
It has been suggested that prenatal exposure to insecticides adversely affects fetal growth, but the overall results have been inconsistent, partly because of the different exposure sources and exposure assessments used. In the French PELAGIE (Perturbateurs Endocriniens: Étude Longitudinale sur les Anomalies de la Grossesse, l'Infertilité et l'Enfance) mother and child cohort (2002-2006), the authors investigated the association between fetal growth and insecticide exposure (n = 1,213) using an integrated Bayesian latent variable model to include multiple exposure sources: agricultural activities, nonorganic diet, household insecticide use on plants, and household insecticide use against insects. They used a questionnaire to collect information on household use and organic diet, and a national agricultural census provided data on agricultural activities in the women's municipalities of residence. A 0.10-cm decrease in head circumference at birth (95% credibility interval: -0.22, 0.01) was associated with fetal insecticide exposure from agricultural activities in the municipality of residence. Decreases in average birth weight (-27 g; 95% credibility interval: -59, 6) and head circumference (-0.12 cm; 95% credibility interval: -0.26, 0.01) were associated with household insecticide use to treat plants. The present results suggest an inverse association between fetal growth and prenatal insecticide exposure from nearby agricultural activity or household use. Bayesian modeling via latent variables is a natural framework for including multiple sources of exposure to environmental pollutants.
ISSN: 0002-9262

hal-00875979
https://hal.archives-ouvertes.fr/hal-00875979
DOI : 10.1093/aje/kwr422
PUBMED : 22534205

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We investigate the contribution of atmospheric and its induced non-tidal oceanic loading effects on surface time-varying gravity and tilt measurements for several stations in Western Europe. The ocean response to pressure forcing can be modelled accordingly to the inverted barometer, i.e. assuming that air pressure variations are fully compensated by static sea height changes, or using ocean general circulation models.Wevalidate two runs of theHUGO-mbarotropic ocean model by comparing predicted sea surface height variations with hundred tide-gauge measurements along the European coasts. We then show that global surface pressure field, as well as a barotropic high-resolution ocean model forced by air pressure and winds allow in most cases a significant reduction of the variance of gravity residuals and, to a smaller extends tilt residuals. Wefinally show that precise gravity measurements with superconducting gravimeters allow the observation of large storm surges, occurring in the North Sea, even for inland stations. However, we also confirm that the continental hydrology contribution cannot be neglected. Thanks to their specific sensitivity feature, only tiltmeters closest to the coast can clearly detect the loading due to these storm surges.
ISSN: 0264-3707

hal-00708046
https://hal.archives-ouvertes.fr/hal-00708046
https://hal.archives-ouvertes.fr/hal-00708046/document
https://hal.archives-ouvertes.fr/hal-00708046/file/ETS2008_BOY.pdf
BIBCODE : 2009JGeo...48..182B

Éditeur(s) : HAL CCSD
Résumé : Two major findings emerge from the theoretical analysis of Transport-Tourism link via a game theory type model of capacity coordination. Firstly the model explains the optimal capacities ratio of Transport and Tourism by the quotient of the ratio of tourism type (ratio of the length of stay in the destination and of transport duration) divided by the installation costs ratio (of transport and tourism).The corollary of this first finding gives the second outcome: The optimal transport and Tourism profit ratio is the product of the ratio of the type of tourism by the index of overcapacity conditions (a non linear combination of installation costs, and durations). From these results, it follows an interpretive grid that allows, according to tourism types, firstly to identify the optimal overcapacities by the difference between installation costs; and secondly the equilibrium ratio of profits according to the overcapacity direction and the tourism types.
Deux résultats ressortent de l’analyse théorique du lien Transport-tourisme via un modèle de coordination des capacités : l’expression et les déterminants des capacités et des profits optimaux relatifs du Transport et du Tourisme. L’article démontre que le rapport des capacités optimales de transport et de tourisme dépend du ratio comparatif de leurs coûts d’installation à celui inversé de leur poids relatif. Ce premier résultat a pour corollaire le second : le rapport d’équilibre des profits est le produit des indicateurs du type de tourisme (le ration des temps respectifs dans le transport et dans la destination) de la destination par celui identifiant les conditions de surcapacité relative. De ces résultats généraux, il suit une grille d’interprétation qui permet d’identifier d’abord le rapport optimal des capacités selon l’écart entre les coûts d’installation et le type de tourisme ; et ensuite le rapport d’équilibre des profits selon les sens des surcapacités relatives et le types de tourisme.
https://hal.univ-antilles.fr/hal-01265818

Droits : info:eu-repo/semantics/OpenAccess
hal-01265818
https://hal.univ-antilles.fr/hal-01265818
https://hal.univ-antilles.fr/hal-01265818/document
https://hal.univ-antilles.fr/hal-01265818/file/TRANP-TOUR.pdf

Éditeur(s) : HAL CCSD Oxford University Press (OUP)
Résumé : International audience
Anisotropy of low-field magnetic susceptibility (AMS) of basaltic lava flows can give some clues about post-emplacement tilting occurring in volcanic sequences. Such a study has been carried out on a sequence of 19 successive lava flows from Kerguelen Archipelago. Surprisingly, two different patterns were observed. The first one - herein called normal fabric - is consistent with the lava-flow direction inferred from geological observations, whereas the second one observed for about 70 per cent of the analysed samples - herein called abnormal fabric - appears to be unrelated to the shear history of the lava flows during their emplacements. These abnormal fabrics are not strictly inverse fabric but seem to have a more complex origin. The unusual nature of these abnormal fabrics has been confirmed by lattice preferred orientation of plagioclases obtained from high-resolution electron backscattered diffraction measurements. The aim of this study is to propose a physical interpretation of these fabrics. A first step in our understanding was to clearly identify the nature and the magnetic properties of the Fe-Ti oxides assemblage. Thus, we present a comprehensive rock magnetic analysis relying on low- and high-temperature thermomagnetic curves (K-T), crossover diagrams, first-order reversal curves, ore-microscopy, Mössbauer measurements and electron backscattered images. We found that in the present case the abnormal fabrics are probably linked to a mixture of prevailing single domain (SD) strongly interacting grains population and a subsidiary multidomain grains population. SD grains are identified as small magnetite crystallized within the interstitial glass in globular aggregates along the silicate framework. Then a question arises: to what extent such SD interacting grains in globular aggregates can affect the magnetic susceptibility and its anisotropy? To answer this question, we developed a physical model in which the total energy density of an SD grain with an uniaxial anisotropy is minimized. In this model, the distribution function of the direction of the magnetic interaction field is comprised between two boundary states. It is either isotropic, which formally corresponds to the thermal demagnetized state, or it is ordered, which formally corresponds to the Alternative Field demagnetized state. We show that in both cases the degree of anisotropy decreases as the interaction field increases. Thus, we conclude that the abnormal fabric encountered in this study can be simply explained by strong magnetostatic interactions that would explain the large scattering of AMS often observed in basaltic lava flows.
ISSN: 0956-540X

hal-00716449
https://hal.archives-ouvertes.fr/hal-00716449
https://hal.archives-ouvertes.fr/hal-00716449/document
https://hal.archives-ouvertes.fr/hal-00716449/file/gji-S-12-HAL.pdf
DOI : 10.1111/J.1365-246X.2012.05421.X

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The interseismic velocity field provided by geodetic methods is generally interpreted in the framework of a thick elastic lithosphere with a slipping fault at depth. Because lateral variations of lithospheric rheology play a key role in determining the geological strain distribution, I examine the idea that interseismic strain rate variations also occur in response to lateral variations in the elastic thickness of the lithosphere. Using a stress balance principle and some simplifying assumptions, I show using a 1D model that elastic thickness is inversely proportional to strain rate for the simple case of pure strike-slip faulting. Elastic thickness computed on three profiles crossing the San Andreas fault system (SAFS) suggests that the distribution of interseismic strain rate is compatible with a thick elastic lithosphere in the Great Basin-Sierra Nevada province and on the Pacific plate. Conversely, a thin plate with a shallow asthenosphere is needed on the SAFS to explain its high strain rate. A 2.5D Finite Element model of interseismic strain in the Carrizo Plain region in Central California shows how known vertical and horizontal variations of elastic properties refine 1D model predictions. In a case of a multiple fault system, I point out that the interseismic velocity is not causally tied to faults slip rate. Therefore, analysing the velocity field across the SAFS cannot reliably provide faults slip rate distribution as previously claimed. Rather, the apparent correlation between geologic slip rate and interseismic strain may only indicate that the elastic thickness plays a dominant role in controlling fault strength. Finally, I suggest that interseismic geodetic strain could be a new way to infer effective elastic plate thickness on the continents.
ISSN: 0012-821X

hal-00412155
https://hal.archives-ouvertes.fr/hal-00412155
DOI : 10.1016/j.epsl.2008.01.046

Éditeur(s) : HAL CCSD
Résumé : International audience
Optimizing the resource extraction and limiting the environmental constraint motivate to accurately characterize reservoirs. The extraction of resources induces volume change of the reservoir causing displacements in the surrounding medium up to the surface. The resulting surface deformation is usually significant enough to be measurable by geodetic instruments (GPS, satellites, tiltmeters, strainmeters). However, the data needs to be associated to a reservoir model using an inverse scheme to allow the estimation of physical properties of the reservoir. Complete geodetic data including InSAR, GPS, tilt, strain and gravimetric data are uncommon for conventional, unconventional or mining exploitations. In this study, we work on the one site that gathers a wide range of geodetic data: the salt exploitation of Vauvert, France, operated by KemOne. Our approach aims at estimating the volume changes of the cavities created by the extraction combining all the available geodetic data. To do so, we minimize a global functional including weighting factors for each data type. The weighting factors are optimally estimated for our study and can be adapted depending on the issue. Hence, an optimal distribution of data can be suggested for a specific reservoir characterization.
79th EAGE Conference
Paris, France

Droits : http://hal.archives-ouvertes.fr/licences/copyright/
hal-01575426
https://hal.archives-ouvertes.fr/hal-01575426
https://hal.archives-ouvertes.fr/hal-01575426/document
https://hal.archives-ouvertes.fr/hal-01575426/file/reservoir-characterization-inversion.pdf
DOI : 10.3997/2214-4609.201700987

Éditeur(s) : HAL CCSD
Résumé : National audience
Objectif L’objectif était d’identifier des formes d’organisation du travail et d’étudier leur association avec les douleurs de l’épaule et le syndrome de la coiffe des rotateurs (SCR) chez les salariés, à partir des données du programme de surveillance épidémiologique des troubles musculo-squelettiques mis en œuvre dans les Pays de la Loire. Méthodes Entre 2002 et 2005, la participation volontaire de 83 médecins du travail a permis d’inclure par tirage au sort 3710 salariés lors de leur visite médicale périodique. Seize variables organisationnelles ont été recueillies par auto-questionnaire. Les symptômes de l’épaule ont été recueillis à l’aide d’un questionnaire de type nordique et le SCR a été diagnostiqué par le médecin à l’aide d’un examen clinique standardisé. Une classification ascendante hiérarchique (CAH) des variables organisationnelles puis des salariés ont permis d’identifier les différentes formes d’organisation du travail. Les associations entre les formes d’organisation du travail et les douleurs de l’épaule et le SCR ont été étudiées par des régressions logistiques ajustées sur des facteurs individuels, biomécaniques et psychosociaux. Résultats Cinq classes d’organisation du travail ont été identifiées. Une classe de salariés s’est révélée fortement exposée aux contraintes organisationnelles : – travail en équipe postée ; – polyvalence ; – faible latitude décisionnelle ; – répétitivité des tâches ; – rythme de travail imposé par : – le déplacement automatique d’un produit ou d’une pièce/la cadence automatique d’une machine, – la dépendance immédiate vis-à-vis du travail des collègues, – des normes de production ou des délais à respecter, – des contrôles ou une surveillance permanents. À l’inverse, elle était moins exposée au rythme de travail imposé par une demande extérieure (public, client) que l’ensemble de l’échantillon. Par rapport à cette classe, les salariés des quatre autres classes avaient un risque plus faible de douleurs de l’épaule au cours des 12 derniers mois (OR de 0,6 [0,5–0,7] à 0,8 [0,6–0,9]), permanentes au cours des 12 derniers mois (OR de 0,6 à 0,8 [0,5–1,0]) et au cours des 7 derniers jours (OR de 0,6 [0,4–0,9], à 0,8 [0,6–1,0]). L’association était non significative pour le SCR (p = 0,11). Conclusions L’étude a montré une association significative entre les douleurs de l’épaule et l’exposition à des contraintes organisationnelles. Ces résultats seront à confirmer à l’aide de modèles à équations structurelles
16e colloque scientifique de l’ADEREST
Lyon, France

hal-01187141
https://hal-univ-rennes1.archives-ouvertes.fr/hal-01187141
DOI : 10.1016/j.admp.2015.04.036

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
A hallmark of living systems is the management and the storage of information through genetic and epigenetic mechanisms. Although the notion of epigenetics was originally given to any regulation beyond DNA sequence, it has often been restricted to chromatin modifications, supposed to behave as cis-markers, specifying the sets of genes to be expressed or repressed. This definition does not take into account the initial view of epigenetics, based on nonlinear interaction networks whose "attractors" can remain stable without need for any chromatin mark. In addition, most chromatin modifications are the steady state resultants of highly dynamic modification and de-modification activities and, as such, seem poorly appropriate to work as long-term memory keepers. Instead, the basic support of epigenetic memory could remain the attractors, to which chromatin modifications belong as do many other components. The influence of chromatin modifications in memory is highly questionable when envisioned as static structural marks, but can be recovered under the dynamic circuitry perspective, thanks to their self-templating properties. Beside their standard repressive or permissive functions, chromatin modifications can also influence transcription in multiple ways such as: (1) by randomizing or inversely stabilizing gene expression, (2) by mediating cooperativity between pioneer and secondary transcription factors, and (3) in the hysteresis and the ultrasensitivity of gene expression switches, allowing the cells to take unambiguous transcriptional decisions.
ISSN: 1420-682X

hal-01063617
https://hal.archives-ouvertes.fr/hal-01063617
DOI : 10.1007/s00018-012-0923-7
PUBMED : 22331281

Éditeur(s) : HAL CCSD Springer Verlag
Résumé : International audience
Smoking only partly explains the higher lung cancer incidence observed among socially deprived people. Occupational exposures may account for part of these inequalities, but this issue has been little investigated. We investigated the extent to which smoking and occupational exposures to asbestos, silica and diesel motor exhaust mediated the association between education and lung cancer incidence in men. We analyzed data from a large French population-based case–control study (1976 lung cancers, 2648 controls). Detailed information on lifelong tobacco consumption and occupational exposures to various carcinogens was collected. We conducted inverse probability-weighted marginal structural models. A strong association was observed between education and lung cancer. The indirect effect through smoking varied by educational level, with the strongest indirect effect observed for those with the lowest education (OR = 1.34 (1.14–1.57)). The indirect effect through occupational exposures was substantial among men with primary (OR = 1.22 (1.15–1.30) for asbestos and silica) or vocational secondary education (OR = 1.18 (1.12–1.25)). The contribution of smoking to educational differences in lung cancer incidence ranged from 22 % (10–34) for men with primary education to 31 % (−3 to 84) for men with a high school degree. The contribution of occupational exposures to asbestos and silica ranged from 15 % (10–20) for men with a high school degree to 20 % (13–28) for men with vocational secondary education. Our results highlight the urgent need for public health policies that aim at decreasing exposure to carcinogens at work, in addition to tobacco control policies, if we want to reduce socioeconomic inequalities in the cancer field.
ISSN: 0393-2990

hal-01360240
http://hal.upmc.fr/hal-01360240
http://hal.upmc.fr/hal-01360240/document
http://hal.upmc.fr/hal-01360240/file/Menvielle_2016_Quantifying_the.pdf
PUBMED : 27417979

Éditeur(s) : HAL CCSD Geological Society of London
Résumé : International audience
Low-velocity zones ('bright spots') imaged by the INDEPTH seismic experiment in southern Tibet are extensively interpreted as widespread partial melt within the crust, which has given a strong support for the channel flow model. These suggest that a continuous seismic low-velocity zone underlies Tibet on the large scale. Here we take advantage of the Hi-CLIMB seismic experiment which includes a dense south-north profile and a lateral 2D seismic network to assess the vertical and the horizontal extension of low-velocity zones in southern Tibet. Several approaches including migration, amplitude analysis and waveform inversion of receiver functions are performed to detect crustal low-velocity zones using this new seismological dataset. Our results reveal localized and discontinuous low-velocity zones in Tibet. They indicate that the vertical extension of the low-velocity zones is about 10 km, and their maximum horizontal length appears to be c. 50 km. Our study suggests a partial correlation between the location of these low-velocity zones and the spatial distribution of Tibetan grabens. These results, especially the non-continuity of low-velocity zones, together with the observed regular value of mean crustal VP/VS ratio, question the existence of widespread partial melt of the southern Tibetan crust and, therefore, the viability of the channel flow model.
Growth and Collapse of the Tibetan Plateau

hal-00853971
https://hal.archives-ouvertes.fr/hal-00853971
DOI : 10.1144/SP353.6