Éditeur(s) : HAL CCSD INRP/ENS éditions
Résumé : International audience
Cet article se propose d’étudier les positionnements des enseignants et des élèves face à l’évaluation, ainsi que la manière dont les élèves interprètent la posture de l’enseignant. Plus précisément, il s’agit d’examiner les variabilités interclasse et intraclasse en ce qui concerne les postures des enseignants et des élèves. L’objectif est d’identifier les classes dans lesquelles les acteurs scolaires ont des conceptions convergentes, l’hypothèse étant que, dans ce cas, un espace commun de conceptions évaluatives réunirait les élèves et leurs enseignants. Dans la foulée, il s’agit également d’étudier dans quelles classes les élèves perçoivent les conceptions des enseignants de manière exacte. Les résultats mettent en évidence différents profils de positionnement chez les enseignants et les élèves ; ces profils se ressemblent fortement. Par ailleurs, on retrouve peu de classes à l’intérieur desquelles les points de vue des acteurs sont en concordance.
ISSN: 0556-7807

hal-01532843
https://hal.univ-antilles.fr/hal-01532843

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The Betic-Rif orocline surrounding the Alboran Sea, the westernmost tip of the Mediterranean Sea, accommodates the NW–SE convergence between the Nubia and Eurasia plates. Recent GPS observations indicate a ∼4 mm/yr SW motion of the Rif Mountains, relative to stable Nubia, incompatible with a simple two-plate model. New gravity data acquired in this study define a pronounced negative Bouguer anomaly south of the Rif, interpreted as a ∼40 km-thick crust in a state of non-isostatic equilibrium. We study the correlation between these present-day kinematic and geodynamic processes using a finite-element code to model in 2-D the first-order behavior of a lithosphere affected by a downward normal traction (representing the pull of a high-density body in the upper mantle). We show that intermediate viscosities for the lower crust and uppermost mantle (View the MathML source1021–1022Pas) allow an efficient coupling between the mantle and the base of the brittle crust, thus enabling (1) the conversion of vertical movement, resulting from the downward traction, to horizontal movement and (2) shortening in the brittle upper crust. Our results show that incipient delamination of the Nubian continental lithosphere, linked to slab pull, can explain the present-day abnormal tectonics, contribute to the gravity anomaly observed in northern Morocco, and give insight into recent tectonics in the Western Mediterranean region.
ISSN: 0012-821X

hal-01467130
https://hal.archives-ouvertes.fr/hal-01467130
DOI : 10.1016/j.epsl.2016.08.041

Éditeur(s) : HAL CCSD Taylor & Francis (Routledge)
Résumé : International audience
The influences of task difficulty (index difficulty: 2-4), input device of different length, range of motion and mode of resistance (joystick or rotorcraft stick), and directions of movement (leftward rightward) on motor patterns in a realistic control situation were examined with a multilevel analysis (joint kinematics and muscular variables, and global task performance). Eight subjects controlled the displacements of a virtual object during a slalom task characterized by a realistic inertial model. Pilots adapted the endpoint kinematic organization to increasing accuracy constraints to preserve task success whatever the device and the direction. However, the rotorcraft stick manipulation remains highly complex in comparison to the joystick due to poorer proprioceptive information, higher inertial constraints, and an asymmetrical muscle control.
ISSN: 0022-2895

hal-01442056
https://hal.archives-ouvertes.fr/hal-01442056
https://hal.archives-ouvertes.fr/hal-01442056/document
https://hal.archives-ouvertes.fr/hal-01442056/file/Fuente%20-%20J%20Motor%20Behav%20-%202013.pdf
DOI : 10.1080/00222895.2013.837424

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
The ∼55 km-long Firouzkuh fault is located in the Central Alborz Mountains of Iran. It is a left-lateral fault, which dips to the south, and possesses a small dip-slip component of motion that we interpret to result from extension. The ratio of horizontal to vertical displacement across the fault, calculated from the cumulative displacement of landscape features, is 7.6. We provide constraints on the timing of the last earthquake on the Firouzkuh fault from two trenches (T1 and T2) across the fault zone, excavated in 2004, and located east of Firouzkuh city. The trenches expose faulted sedimentary deposits. Two optically-stimulated luminescence (OSL) ages from sediments in the lower part of trench T1 date from the late Pleistocene (15.9 ± 0.9 ka and 27.1 ± 1.7 ka). The younger of the two dated units in T1 is displaced vertically across the fault by 2.2–4.4 m, from which we estimate a strike-slip displacement of 18.2–33.4 m, and hence a average horizontal slip-rate of 1.1–2.2 mm/yr. The sediments exposed in T1 do not yield constraints on the most recent earthquake history. In trench T2, however, human skeletal remains of a middle aged male, which yield a radiocarbon age of 1159 ± 28 BP (corresponding to a mean calendar age of 791 AD), were found within a faulted alluvial layer at a depth of 60–70 cm from the surface. The existence of these medieval human places shows that a surface-rupturing earthquake occurred at some time after 1159 ± 28 BP. The amount of slip in each earthquake on the Firouzkuh fault is difficult to estimate, but assuming the entire ∼55 km fault length ruptures in each event, they will have had a maximum magnitude of 7.1. At our estimated late Quaternary slip-rate of ∼1.1–2.2 mm/yr magnitude 7.1 earthquakes, involving ∼1.2 m average displacement, would be expected to occur every ∼1100–540 years. As the last earthquake on the Firouzkuh fault may be up to ∼700 years in age we suggest that the Firouzkuh fault is a major hazard for earthquakes in the near future.
ISSN: 0743-9547

hal-01122835
https://hal.archives-ouvertes.fr/hal-01122835
DOI : 10.1016/j.jseaes.2013.12.018

Éditeur(s) : HAL CCSD Geological Society of America
Résumé : International audience
Hollingsworth et al. (2008) propose that the westward motion of the South Caspian basin started 10 Ma ago. This is earlier than the ca. 5 Ma proposed by Axen et al. (2001) and Allen et al. (2002), and substantially earlier than the ca. 1.5 Ma proposed by Ritz et al. (2006). This new interpretation is based on the assumption that the present tectonics pattern (geometry of faults, slip vectors, and slip rates) did not vary through time.
ISSN: 0091-7613

hal-00854468
https://hal.archives-ouvertes.fr/hal-00854468
DOI : 10.1130/G25627C.1

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : International audience
The two experiments reported in the present paper concern (i) the differential imagery value of French and Creole and (ii) the influence of language on the recall of sequences of patterned movements in a bilingual population. Creole words were obtained a higher imagery value than French words, certainly because Creole is an oral and vernacular language. Motor recall scores were better when the sequence was presented in Creole compared to French. The generation of visual images by Creole would facilitate the memorization and recall of new sequences of movements. The effect of language on imagery value of words and motor recall among bilingual French–Creole subjects was discussed in terms of nature of information encoding in each language.
Les deux expérimentations relatées dans cet article évaluent la valeur d'imagerie de mots et le rappel moteur d'enchaînements auprès de bilingues français–créole en faisant varier la langue de présentation. Les mots en créole, supposés susciter plus facilement des images mentales visuelles, car le créole est une langue orale et vernaculaire, ont effectivement obtenu une cote plus élevée que les mots français sur l'échelle de valeur d'imagerie. L'évocation d'images visuelles facilitant la mémo-risation et la planification de séquences de mouvements, les performances de rappel obtenues à partir des consignes en créole ont été supérieures à celles obtenues en français. Les effets de la langue de présentation sur la valeur d'imagerie des mots et le rappel moteur d'enchaînements de morphocinè-ses auprès des participants bilingues sont discutés en termes de nature d'encodage de l'information verbale dans chacune des langues.
ISSN: 0033-2984

hal-01540163
https://hal.univ-antilles.fr/hal-01540163
DOI : 10.1016/j.psfr.2005.05.011

Éditeur(s) : HAL CCSD Elsevier Masson
Résumé : In Vietnam, the Triassic Indosinian collision affected coevally the Truong Son belt and the Kontum Massif,which were not independent tectonic units, but parts of the same Gondwana-derived Indochina continental block. This thermotectonic event took place synchronously throughout Vietnam, during the Lower Triassic 250-240-Ma time interval, as demonstrated by numerous geochronological data, combining Ar-Ar and U-Pb dating methods. Structural and kinematic investigations, in the Indosinian metamorphic rocks, reveal that the collisional process resulted from a consistent northwest-striking convergence of Indochina with respect to the adjacent blocks. It is suggested that this motion was taken up by a pair of opposite subduction zones: to the north, beneath South China, and to the west, beneath western Indochina, along the Song Ma and Po Ko sutures, respectively. Tectonic markers, calc-alkaline subduction-related volcanism and granitic intrusions and the generation of high-pressure rocks that have been recently discovered support this geodynamic setting, at least along Po Ko. Along the northwest-trending Song Ma zone, the obliquity of the convergence during subduction and subsequent collision resulted in the development, within the Truong Son Belt, of a set of subparallel dextral mylonitic shear zones, under amphibolite-facies metamorphism. The intermediate segments remained weakly metamorphic or even almost devoid of metamorphism. Along Po Ko, the convergence was near-orthogonal, with a left-lateral strike-slip component; the ongoing continental subduction resulted in the reworking of the Kontum granulitic basement and the development of Indosinian HP granulitic conditions; the subsequent extension-related exhumation operated approximately in the same northwestwards direction. This Indosinian evolution, applied on a continental crust that had been probably affected, as in South China, by a Caledonian-related event, as judged by the general unconformity of the Lower Devonian sediments, the widespread occurrence of magmatic crystallisation ages of ca 450 Ma (Ordovician-Silurian), and by the approximately similar age of the primary granulitic episode in the Kontum Massif. The similarities of the Devonian facies over central, northern Vietnam and South China imply a land connection, possibly as a consequence of a Caledonian collision along Song Ma, but this does not preclude a further oceanic opening and a closure during the Indosinian.
ISSN: 1631-0713

hal-00411591
https://hal.archives-ouvertes.fr/hal-00411591
DOI : 10.1016/j.crte.2007.10.005

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
Active faults from the Campo de Dalías (SE Betic Cordillera) allow us to constrain the deformation styles involved in the development of segmented oblique-slip faults. This sector constitutes the widest outcrop of Plio-Quaternary sediments in the northern boundary of the Alboran Sea. It has emerged since the Late Pliocene, and therefore provides recent deformation markers that are not disturbed by erosive processes. The faults started to grow during the Pleistocene, reactivating previous hybrid joints, with a normal-dextral slip. We present a detailed map of the largest fault in the area, the Loma del Viento fault, comprising six onshore segments. Based on field work and aerial photography, the distributions of the contiguous joints have been mapped, and the joints reactivated as faults are identified. Some of these fault segments are hard-linked, and fault slip enhances toward the linkage sectors between them with associated sedimentary depocenters. An electrical tomography profile reveals the wedge geometry of a unit of Pleistocene conglomerates and red silts that were coevally deposited during the fault movement. Long-term slip rate in the central part of the fault is estimated at 0.07 ± 0.03 mm/y. In addition, a seismic crisis nucleated close to the Loma del Viento fault during November 2010 was recorded. Moment tensor analysis of the two mainshocks (Mw 3.5 and 4.2) provides a focal solution indicating a N120°E striking right-lateral strike-slip fault. The corrugated morphology of the Loma del Viento fault may have influenced its seismic behavior. Some of the fault segments are oblique to the general motion of the fault. These oblique segments would provide higher resistance against the general fault motion and could lock the fault, leading to accumulate elastic energy.
ISSN: 0040-1951

hal-00750357
https://hal.archives-ouvertes.fr/hal-00750357
DOI : 10.1016/j.tecto.2011.12.001

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
A variety of atypical plume-like structures and focused upwellings that are not rooted in the lower mantle have recently been discussed, and seismological imaging has shown ubiquitous small-scale convection in the uppermost mantle in regions such as the Mediterranean region, the western US, and around the western Pacific. We argue that the three-dimensional return flow and slab fragmentation associated with complex oceanic subduction trajectories within the upper mantle can generate focused upwellings and that these may play a significant role in regional tectonics. The testable surface expressions of this process are the outside-arc alkaline volcanism, topographic swell, and low-velocity seismic anomalies associated with partial melt. Using three-dimensional, simplified numerical subduction models, we show that focused upwellings can be generated both ahead of the slab in the back-arc region (though -five times further inward from the trench than arc-volcanism) and around the lateral edges of the slab (in the order of 100 km away from slab edges). Vertical mass transport, and by inference the associated decompression melting, in these regions appears strongly correlated with the interplay between relative trench motion and subduction velocities. The upward flux of material from the depths is expected to be most pronounced during the first phase of slab descent into the upper mantle or during slab fragmentation. We discuss representative case histories from the Pacific and the Mediterranean where we find possible evidence for such slab-related volcanism.
ISSN: 0012-821X

hal-00553075
https://hal.archives-ouvertes.fr/hal-00553075
DOI : 10.1016/j.epsl.2010.08.012

Éditeur(s) : HAL CCSD
Résumé :  
absent
Xemes Journées d'Ecoligie Fonctionnelles
La Grande Motte, France

hal-01032090
https://hal.archives-ouvertes.fr/hal-01032090

Éditeur(s) : Université des Antilles Études caribéennes
Résumé : Concevoir le tourisme comme un outil de lutte contre la pauvreté nécessite en premier lieu de s’entendre sur le sens du mot pauvreté et de clarifier les intentions politiques d’un tel projet. La réflexion sur la réduction de la pauvreté grâce au tourisme peut être synthétisée en trois temps : tout d’abord, les effets bénéfiques du ruissellement des revenus touristiques dans les sociétés d’accueil, ensuite les dommages collatéraux qui résultent du tourisme et, finalement, définir les conditions nécessaires pour intégrer favorablement le projet touristique dans les territoires hôtes. Au final, il apparaît indispensable de développer une politique volontariste, car le fameux ruissellement de revenus ne va pas naturellement profiter aux plus démunis. Compte tenu des impacts complexes et contradictoires du tourisme international (notamment en matière d’inflation, de fuites des revenus, de déstructuration accélérée des sociétés locales), il faut l’inscrire dans un projet d’un territorial cohérent et soutenu par les communautés locales afin de dégager de réels bénéfices.
Develop tourism as a tool in the fight against poverty requires first to agree on the meaning of the word poverty and to clarify the political intentions of the project. Reflection on the reduction of poverty through the tourism can be synthesized in three steps: first, the beneficial effects of runoff from tourist revenues in host societies, then the collateral damage resulting from tourism and, finally, to define the conditions necessary to integrate positively tourism project in the host territories.In the end, it is indispensable to develop a proactive policy, because the poorest will not benefit from famous income runoff. Taking into account complex and contradictory impact of international tourism (including inflation, revenue leakage, deconstruction accelerated of local societies), it is necessary to include it in a sustained and coherent territorial project by local communities to identify real benefits.

Droits : info:eu-repo/semantics/openAccess
urn:doi:10.4000/etudescaribeennes.6601
http://journals.openedition.org/etudescaribeennes/6601

Éditeur(s) : HAL CCSD
Résumé : From the protolanguage born with Homo erectus, the modern human language of Homo sapiens has naturally diversified into tonal, stress-timed, or syllable-timed languages, although the definition of the syllable has yet to be established. Thus for a French speaker, the transition from a language punctuated by the syllable to a language punctuated by the lexical stress will be a delicate point in learning oral English. For this purpose, we recommend the implementation of a reprogramming of the articulatory gesture in the brains as evidenced by articulatory phonology. Through the arched beam, Broca's area of the French-speaking learner will inhibit the French-related data to send to Wernicke's area new information regarding the reception / production of oral English.
A partir du protolangage né avec Homo erectus, le langage humain moderne d'Homo sapiens s'est naturellement diversifié en langues tonales, accentuelles, ou syllabiques, bien que la définition de la syllabe reste encore à établir. Ainsi pour un francophone, le passage d'une langue rythmée par la syllabe à une langue rythmée par l'accent lexical sera un point délicat de l'apprentissage de l'anglais oral. Pour ce faire, nous préconisons la mise en place d'une reprogrammation de la gestuelle articulatoire telle qu'elle a pu être mise en évidence par la phonologie articulatoire. Par le biais du faisceau arqué, l'aire de Broca de l'apprenant francophone inhibera les données liées au français pour envoyer à l'aire de Wernicke de nouvelles informations quant à la réception / production de l'anglais oral. Mots clés : neurodidactique, anglais oral, phonologie articulatoire, aires du langage, mémoire procédurale et à long terme. Abstract: From the protolanguage born with Homo erectus, the modern human language of Homo sapiens has naturally diversified into tonal, stress-timed, or syllable-timed languages, although the definition of the syllable has yet to be established. Thus for a French speaker, the transition from a language punctuated by the syllable to a language punctuated by the lexical stress will be a delicate point in learning oral English. For this purpose, we recommend the implementation of a reprogramming of the articulatory gesture in the brains as evidenced by articulatory phonology. Through the arched beam, Broca's area of the French-speaking learner will inhibit the French-related data to send to Wernicke's area new information regarding the reception / production of oral English.
https://hal.archives-ouvertes.fr/hal-01626540

hal-01626540
https://hal.archives-ouvertes.fr/hal-01626540
https://hal.archives-ouvertes.fr/hal-01626540/document
https://hal.archives-ouvertes.fr/hal-01626540/file/Neurodidactique%20%20Comment%20le%20cerveau%20d%27un%20apprenant%20francophone%20peut-il%20se%20programmer%20sur%20une%20langue%20accentuelle..pdf

Éditeur(s) : HAL CCSD Elsevier
Résumé : Le titre a été changé Ancien titre: Roles for local crowding and pressure in counteracting density fluctuations at equilibrium
International audience
What is the probability that all the gas in a box accumulates in the same half of this box? Though amusing, this question underlies the fundamental problem of density fluctuations at equilibrium, which has profound implementations in many physical fields. The currently accepted solutions are derived from the studies of Brownian motion by Smoluchowski, but they are not appropriate for the directly colliding particles of gases. Two alternative theories are proposed here using self-regulatory Bernoulli distributions. A discretization of space is first introduced to develop a mechanism of matter congestion holding for high densities. In a second mechanism valid in ordinary conditions, the influence of local pressure on the location of every particle is examined using classical laws of ideal gases. This approach reveals that a negative feedback results from the reciprocal influences between individual particles and the population of particles, which strongly reduces the probability of atypical microstates. Finally, a thermodynamic quantum of time is defined to compare the recurrence times of improbable macrostates predicted through these different approaches.
Physica A: Statistical Mechanics and its Applications

hal-00920985
https://hal-univ-rennes1.archives-ouvertes.fr/hal-00920985
https://hal-univ-rennes1.archives-ouvertes.fr/hal-00920985v2/document
ARXIV : 1404.6223
DOI : 10.1016/j.physa.2014.03.067

Éditeur(s) : HAL CCSD
Résumé : The literature has identified a set of factors explaining the accumulation of capital. However, little attention has been paid to the impact of cultural beliefs. This paper, based on economic science, uses data collected from 207 haitian formal sector firms to develop and test a model of capital accumulation integrating socio-cultural traits, including life in the present moment, fatalism, primacy of the hereafter and mutual assistance. The results reveal that the primacy of the beyond, life in the present moment and mutual aid have negative and significant impacts on accumulation of capital. And, fatalism has positive and significant effects on this variable.
La littérature a identifié un ensemble de facteurs expliquant l'accumulation du capital. Cependant, les travaux ne se sont que très peu intéressés à l'impact des croyances culturelles. Ce papier, relevant de la science économique, utilise des données collectées auprès de 207 entreprises du secteur formel haïtien pour élaborer et tester un modèle d'accumulation du capital intégrant des traits socioculturels, notamment la vie dans l'instant présent, le fatalisme, la primauté de l'au-delà et l'entraide mutuelle. Les résultats révèlent que la primauté de l'au-delà, la vie dans l'instant présent et l'entraide mutuelle ont des impacts négatifs et significatifs sur l'accumulation du capital. En revanche, le fatalisme a des effets positifs et significatifs sur cette variable. Mots clés. Accumulation du capital, croyances, traits socioculturels.
https://hal.univ-antilles.fr/hal-01555285

Droits : info:eu-repo/semantics/OpenAccess
hal-01555285
https://hal.univ-antilles.fr/hal-01555285
https://hal.univ-antilles.fr/hal-01555285/document
https://hal.univ-antilles.fr/hal-01555285/file/Eliccel%20PAUL_%20Croyances%20et%20accumulation%20du%20capital_EP_28_06_17.pdf

Éditeur(s) : HAL CCSD
Résumé : SilviLaser 2015, La Grande Motte, FRA, 28-/09/2015 - 30/09/2015
International audience
The study provides technical guidelines to optimize sampling design parameters in the context of the implementation of biomass predictive models from airborne lidar data. Parameters under study were those easily controlled when implementing an area-based approach, i.e. lidar pulse density and both field sampling protocols and measurements. Parameters most impacting the model accuracy were identified by conducting a one-factor- at -a-time and a global sensitivity analyses. Number and size of field plot, and plot center position accuracy were identified to be the parameters most impacting model accuracy.
Proceedings of silviLaser 2015. Durrieu S. et Véga, C. (eds)
La Grande Motte, France

hal-01286833
https://hal.archives-ouvertes.fr/hal-01286833
https://hal.archives-ouvertes.fr/hal-01286833/document
https://hal.archives-ouvertes.fr/hal-01286833/file/mt2015-pub00046522.pdf
IRSTEA : PUB00046522

Éditeur(s) : HAL CCSD Elsevier
Résumé : A combination of statistical studies on present-day subduction zones and three-dimensional (3D) laboratory models is performed with the aim to clarify the way that plate kinematics control the geometry of the slab and the overriding plate deformation in subduction zones. In 3D laboratory models, the analogue of a two layer linearly viscous lithosphere–upper mantle system is achieved by means of silicon putty glucose syrup tank experiment. The subducting and overriding plate velocities are systematically changed by exploring the variability field of natural plate kinematics. Both statistical and modelling approaches recognize the importance of overriding plate motion on subduction process behavior: (1) trenches migrate at a rate close to the overriding plate motion, but always move slower than the overriding plates. The mechanism at work is a direct consequence of “slab anchoring” opposed by both lithosphere and mantle viscous resistance and is responsible for overriding plate deformation and slab geometry variability. (2) An overriding plate shortens when the overriding plate moves toward the trench and conditions that are favourable for overriding plate extension are created when the overriding plate moves away from the trench. (3) Shallow and steep dips are found if the overriding plate moves toward and away from the trench, respectively.
ISSN: 0012-821X

hal-00406598
https://hal.archives-ouvertes.fr/hal-00406598
DOI : 10.1016/j.epsl.2007.02.004

Éditeur(s) : HAL CCSD American Geophysical Union
Résumé : International audience
We investigate upper mantle anisotropy beneath the Pyrenean range along three N-S profiles across the mountain belt. The results of a first profile that operated in 1993 in the central part of the belt have been presented elsewhere. We present the results of two other profiles that ran in 1995-1996 and 1996-1997 in the eastern and western part of the belt, respectively and propose an interpretation of the whole results. Teleseismic shear waves (SKS, SKKS, and PKS) are used to determine splitting parameters: the fast polarization direction φ and the delay time δt. Teleseismic shear wave splitting in the eastern Pyrenees displays homogeneous φ values trending N100°E and δt values in the range 1.1 to 1.5 s. A station located in the southern Massif Central, 100 km north of the range, is characterized by different splitting parameters (φ = N70°E, δt = 0.7 s). In the western part of the belt, anisotropy parameters are similar across the whole belt (φ = N110°E and δt = 1.3 to 1.5 s). Most of the measured delay times, including those obtained in the central part of the range, are above the global average of the SKS splitting (around 1 s). At the belt scale, φ is generally poorly correlated with recent estimations of the absolute plate motion, which predicts a fast direction ranging between N50°E and N80°E. Instead, the orientation of φ (N100°E) is parallel to the trend of the Pyrenean belt but also to Hercynian preexisting structures. This parallelism supports an anisotropy primarily related to frozen or active lithospheric structures. We show that a signature related to the Pyrenean orogeny is likely for the stations located in the internal domains of the belt. By contrast, the anisotropy measured at the stations located on the external parts of the belt could reflect a pre-Pyrenean (Hercynian) deformation. We suggest that a late Hercynian strike-slip deformation is responsible for this frozen upper mantle anisotropy and that the Pyrenean tectonic fabric developped parallel to this preexisting fabric. Finally, no particularly strong splitting is related to the North Pyrenean Fault, commonly believed to represent the plate boundary between Iberia and Eurasia.
ISSN: 2169-9313

hal-01388841
http://hal.univ-reunion.fr/hal-01388841
http://hal.univ-reunion.fr/hal-01388841/document
http://hal.univ-reunion.fr/hal-01388841/file/Barruol_Aniso_Pyr_JGR1998.pdf
DOI : 10.1029/98JB02790

Éditeur(s) : HAL CCSD European Geosciences Union
Résumé : International audience
Earth deformation is a multi-scale process ranging from seconds (seismic deformation) to millions of years (tectonic deformation). Bridging short- and long-term deformation and developing seismotectonic models has been a challenge in experimental tectonics for more than a century. Since the formulation of Reid's elastic rebound theory 100 years ago, laboratory mechanical models combining frictional and elastic elements have been used to study the dynamics of earthquakes. In the last decade, with the advent of high-resolution monitoring techniques and new rock analogue materials, laboratory earthquake experiments have evolved from simple spring-slider models to scaled analogue models. This evolution was accomplished by advances in seismology and geodesy along with relatively frequent occurrences of large earthquakes in the past decade. This coincidence has significantly increased the quality and quantity of relevant observations in nature and triggered a new understanding of earthquake dynamics. We review here the developments in analogue earthquake modelling with a focus on those seismotectonic scale models that are directly comparable to observational data on short to long timescales. We lay out the basics of analogue modelling, namely scaling, materials and monitoring, as applied in seismotectonic modelling. An overview of applications highlights the contributions of analogue earthquake models in bridging timescales of observations including earthquake statistics, rupture dynamics, ground motion, and seismic-cycle deformation up to seismotectonic evolution.
ISSN: 1869-9510

hal-01553120
https://hal.archives-ouvertes.fr/hal-01553120
https://hal.archives-ouvertes.fr/hal-01553120/document
https://hal.archives-ouvertes.fr/hal-01553120/file/rosenau2017.pdf
DOI : 10.5194/se-8-597-2017

Éditeur(s) : HAL CCSD Elsevier
Résumé : International audience
We present evidence that GPS velocity estimates of plate motions and fault slip rates agree to within uncertainties with geologic estimates during the most recent phase of the geologic evolution of the E Mediterranean region (post-Late Miocene). On this basis, we use the GPS differential velocities to estimate the timing of initiation of the principal structures in NW Turkey, the N Aegean Sea, and central Greece, including, the Marmara Sea, the Gulfs of Evia (GoE) and Corinth (GoC). and the Kephalonia Transform fault (KTF). We interpret these ages to indicate that the North Anatolian fault propagated across the N Aegean, opening the GoE and GoC and initiating the KTF, during the past 1-4 Ma. We further suggest that Aegean extension that was earlier more distributed across the Aegean Basin became focused on this new fault system allowing the southern Aegean and Peloponnisos to translate SW with little internal deformation, as observed today with GPS. This change in tectonic configuration may account for the clear geologic evidence for crustal thinning throughout the S Aegean in apparent contradiction with low present-day strain rates. We further show that the low present-day strain rate along the southern edge of the Aegean micro-plate requires substantial aseismic slip along the plate interface below Crete, consistent with the low level of historic, subduction-type earthquakes along this segment of the subduction zone.
ISSN: 0040-1951

hal-00512634
https://hal.archives-ouvertes.fr/hal-00512634
DOI : 10.1016/j.tecto.2009.05.027

Éditeur(s) : HAL CCSD
Résumé : The northern Mirdita ophiolite massifs in Albanian Dinarides formed at a slow-spreading ridge, active during the Jurassic (160–165 Ma). They share a common horizontal Jurassic–Lower Cretaceous sedimentary cover showing that they were not deeply and intrinsically affected by later Alpine thrusting. The western massifs of Mirdita, first oceanic core complex (OCC) and detachment shear zone described in ophiolites, compare with OCCs in slow-spreading ridges and provide continuous exposure of the deep internal structure of this system, revealing its kinematics, thanks to detailed structural mapping in peridotites and gabbros. The Mirdita detachments root in the Moho transition zone (MTZ), a weak zone at the top of asthenospheric mantle, where basaltic melts impregnate dunites. The OCC domes are plagioclase-amphibole–bearing mylonitic peridotites, ∼400 m thick, grading downward within 200 m to harzburgitic mantle. The mylonitic detachments crossed Moho beneath a NNE-SSW–trending ridge. On the western side of OCC domes, the hanging wall of the ridge, crustal gabbros, and basalts are still preserved, despite being deeply affected by hydrothermal alteration. From there, the partially molten MTZ was detached as a shear zone, mixing with lower gabbros. The OCC emerged, migrating upsection and eastward over 5 km. Finally, the OCC front is observed in hornblende-rich syntectonic mylonites derived from upper gabbros and from the overlying former lid. Serpentinization is static within these mylonites. A low-temperature detachment fault is expressed as a sheared antigoritic mélange at the margin of the mylonitic shear zone. Asthenospheric flow in the harzburgitic mantle beneath the ridge of origin has been preserved below the OCC rooting. The dominant asthenospheric flow direction trends parallel to the ridge axis. This mantle flow rotates over 200 m into the low-temperature mylonitic detachments, where OCC motion turns transversal to the ridge. Crystal preferred orientation measurements on six samples point to brown hornblende crystal growth during mylonitic flow and illustrate the change of olivine intra-crystalline slip system in mylonites compared to porphyroclastic harzburgite.
ISSN: 1553-040X

hal-01504440
https://hal.archives-ouvertes.fr/hal-01504440
DOI : 10.1130/GES01383.1