Nappe stacking and first evidence of Late Variscan extension in the Belledonne Massif (External Crystalline Massifs,French Alps)     

Stéphane Guillot  René-Pierre Ménot  Jean-Michel Caron 《Geodinamica Acta》2013,26(2):97-111

Abstract

In the southwestern part of the Belledonne Massif (External Crystalline Massifs, French Alps), superimposition of three distinct crustal units has been interpreted as the consequence of Late Devonian-Early Carboniferous thrusting toward the ENE under typical collisional metamorphic conditions (9–7 kbar, 600–650 °C). Structural relationships between the different units and the kinematic analysis of microstructures suggest that ductile extensional tectonics with a sinistral component towards the southwest is responsible for the late structure of this domain. Extensional tectonics are responsible for the exhumation of the deep level of the nappe pile (Allemont unit) that recorded an earlier HP-LT tectonometamorphic evolution (10 ± 1 kbar, 550 ± 50 °C) and for the syn-kinematic adiabatic decompression path recorded in the two lowest units (Livet and Allemont). Such isothermal decompression may have been related to rapid thinning (~ 3mm y^?1) and led to local decompressional melting at the base of the nappe pile. The thinning is best explained by extensional tectonics processes affecting the previously thickened Variscan crust during the Upper Carboniferous prior to its restoration to normal thickness. © Elsevier, Paris  相似文献   

Estimation of anisotropic hydraulic conductivity using geophysical data in a coastal aquifer of Karnataka,India     

Priyanka Bangalore Nagaraj  Mohan Kumar Mandalagiri Subbarayappa  Vouillamoz Jean-Michel  Johan Hoareau 《水文研究》2021,35(10):e14395

Estimation of hydraulic parameters is essential to understand the interaction between groundwater flow and seawater intrusion. Though several studies have addressed hydraulic parameter estimation, based on pumping tests as well as geophysical methods, not many studies have addressed the problem with clayey formations being present. In this study, a methodology is proposed to estimate anisotropic hydraulic conductivity and porosity values for the coastal aquifer with unconsolidated formations. For this purpose, the one-dimensional resistivity of the aquifer and the groundwater conductivity data are used to estimate porosity at discrete points. The hydraulic conductivity values are estimated by its mutual dependence with porosity and petrophysical parameters. From these estimated values, the bilinear relationship between hydraulic conductivity and aquifer resistivity is established based on the clay content of the sampled formation. The methodology is applied on a coastal aquifer along with the coastal Karnataka, India, which has significant clayey formations embedded in unconsolidated rock. The estimation of hydraulic conductivity values from the established correlations has a correlation coefficient of 0.83 with pumping test data, indicating good reliability of the methodology. The established correlations also enable the estimation of horizontal hydraulic conductivity on two-dimensional resistivity sections, which was not addressed by earlier studies. The inventive approach of using the established bilinear correlations at one-dimensional to two-dimensional resistivity sections is verified by the comparison method. The horizontal hydraulic conductivity agrees with previous findings from inverse modelling. Additionally, this study provides critical insights into the estimation of vertical hydraulic conductivity and an equation is formulated which relates vertical hydraulic conductivity with horizontal. Based on the approach presented, the anisotropic hydraulic conductivity of any type aquifer with embedded clayey formations can be estimated. The anisotropic hydraulic conductivity has the potential to be used as an important input to the groundwater models.  相似文献   

Estimates of surface drifter trajectories in the equatorial Atlantic: a multi-model ensemble approach   总被引：3，自引：3，他引：0  

Robert Bruce Scott  Nicolas Ferry  Marie Drévillon  Charlie N. Barron  Nicolas C. Jourdain  Jean-Michel Lellouche  Edward Joseph Metzger  Marie-Hélène Rio  Ole Martin Smedstad 《Ocean Dynamics》2012,62(7):1091-1109

We compared the estimates of surface drifter trajectories from 1 to 7?days in the equatorial Atlantic over an 18-month period with five eddying ocean general circulation model (OGCM) reanalyses and one observational product. The cumulative distribution of trajectory error was estimated using over 7,000?days of drifter trajectories. The observational product had smaller errors than any of the individual OGCM reanalyses. Three strategies for improving trajectory estimates using the ensemble of five operational ocean analysis and forecasting products were explored: two methods using a multi-model ensemble estimate and also spatial low-pass filtering. The results were insensitive to the method used to create the ensemble estimates, and by most measures, the results were better than the observational product. Comparison of relative skill of the various OGCM reanalyses suggested promising avenues for exploration for further improvements: forcing with higher frequency wind stress and quality control of input data. One of the lowest horizontal resolution OGCMs, with 1/4° longitude horizontal resolution, made the best trajectory estimates. The individual OGCMs were dominated by errors at spatial scales smaller than about 100 to 200?km, i.e., less than the local deformation radius. But buried in those errors were valuable signals that could be retrieved by combining all the OGCM velocity fields to produce a multi-model ensemble-based estimate. This estimate had skill down to spatial scales about 75?km. Results from this study are consistent with previous work showing that ensemble-mean forecast skill is superior to individual forecasts.  相似文献   

Radiative surface temperature and convective flux calculation over crop canopies     

Jean-Paul Lhomme  Nader Katerji  Alain Perrier  Jean-Michel Bertolini 《Boundary-Layer Meteorology》1988,43(4):383-392

The analysis presented in this paper aims at a better understanding of the potential role of radiative temperature, as measured by a radiometer over crops, in sensible heat flux calculation. Defining radiative temperature as the mean temperature of the surfaces viewed by the radiometer (leaves and soil surface) and assuming that an Ohm's law type formula can be used to express sensible heat flux as a function of the difference between air temperature and radiative temperature, the aerodynamic resistance which divides this temperature difference has been analytically defined. The parameters which appear in the resistance expression depend essentially on wind velocity and canopy structure but also on the inclination angle of the radiometer. Finally an experimental verification is presented with data obtained over a potato crop.  相似文献   

Recent fold growth and drainage development: The Janauri and Chandigarh anticlines in the Siwalik foothills, northwest India   总被引：2，自引：4，他引：2  

Bernard Delcaillau  Jean-Michel Carozza  Edgard Laville 《Geomorphology》2006,76(3-4):241-256

The active growth of a fault-and-thrust belt in frontal zones of Himalaya is a prominent topographical feature, extending 2500 km from Assam to Pakistan. In this paper, kinematical analysis of frontal anticlines and spatial mapping of active faults based on geomorphological features such as drainage pattern development, fault scarps and uplifted Quaternary alluvial fans are presented. We analyse the geomorphic and hydrographic expressions of the Chandigarh and the Janauri active anticlines in the NW India Siwaliks. To investigate the morphological scenario during the folding process, we used spatial imagery, geomorphometric parameters extracted from digital elevation models and fieldwork. Folding between the Beas and Sutlej Rivers gives clear geomorphological evidence of recent fold growth, presumably driven by movements of blind thrust faults. Structural style within the Janauri and Chandigarh anticlines is highly variable (fault-propagation folds, pop-up structures and transfer faults). The approach presented here involves analysis of topography and drainage incision of selected landforms to detect growth of active anticlines and transfer faults. Landforms that indicate active folding above a southwest-dipping frontal thrust and a northeast-dipping back-thrust are described. Along-strike differences in ridge morphology are measured to describe the interaction of river channel patterns with folds and thrust faults and to define history of anticline growth. The evolution of the apparently continuous Janauri ridge has occurred by the coalescence of independent segments growing towards each other. By contrast, systematic drainage basin asymmetry shows that the Chandigarh anticline ridge has propagated laterally from NW to SE.  相似文献   

Questioning emissions-based approaches for the definition of REDD+ deforestation baselines in high forest cover/low deforestation countries     

Camille Dezécache  Jean-Michel Salles  Bruno Hérault 《Carbon balance and management》2018,13(1):21

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Semi-automated filtering of data outliers to improve spatial analysis of piezometric data     

Yohann Tremblay  Jean-Michel Lemieux  Richard Fortier  John Molson  René Therrien  Pierre Therrien  Guillaume Comeau  Marie-Catherine Talbot Poulin 《Hydrogeology Journal》2015,23(5):851-868

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Effect of fines content on soil freezing characteristic curve of sandy soils     

Vu  Quoc Hung  Pereira  Jean-Michel  Tang  Anh Minh 《Acta Geotechnica》2022,17(11):4921-4933

Acta Geotechnica - Soil freezing characteristic curve (SFCC) represents the relationship between soil temperature and unfrozen water content of soil during freezing and thawing processes. In this...  相似文献   

Preliminary results about the stability of an intermediate water current   总被引：1，自引：0，他引：1  

Jean-Michel Baey  Dominique Renouard  Gabriel Chabert D'hieres 《Deep Sea Research Part I: Oceanographic Research Papers》1995,42(11-12)

Experiments were run on a 14 m diameter rotating platform to study the stability conditions for a constant volume flow rate current of intermediate water. The flow was introduced in a two-layer system initially at rest in solid body rotation, along the sidewall of the tank, and allowed freely to evolve. A sink collected the intermediate water and thus ensured that the free surface height was constant. Thus the upstream conditions were the rotation rate, the volume flow rate, the density and the initial width of the intermediate current, which was in geostrophic equilibrium when it left the source; i.e. its thickness along the wall at the source was fixed by this condition. The relevant parameters appear to be the Ekman and the Burger numbers. The data collected from the experiments are very consistent, and it appears that there were five typical flow regimes: (1) a stable current along the whole basin; (2) a series of cyclonic vortices attached to the outer edge of the current, with an upstream stable current; (3) a large cyclonic vortex attached to an anticyclonic instability; (4) dipoles shed from the current into the interior fluid; and (5) generation of lenses of intermediate water, similar to meddies. This last result shows that no topographical effect is required to generate such long-lived lenses, which then drift slowly upstream as the dipoles do.  相似文献   

Comparison of wind and wave measurements and models in the Western Mediterranean Sea   总被引：2，自引：0，他引：2  

Fabrice Ardhuin  Luciana Bertotti  Jean-Raymond Bidlot  Luigi Cavaleri  Valentina Filipetto  Jean-Michel Lefevre  Paul Wittmann 《Ocean Engineering》2007,34(3-4):526-541

We have hindcast the wind and wave conditions in the Mediterranean Sea for two one month periods. Four different meteorological models and three different wave models have been used. The results have been compared with satellite and buoy wind and wave observations.Several conclusions concerning both the instruments and the models have been derived. The quality of both wind and wave results has been assessed. Close to the coasts high resolution, nested wave models are required for sufficient reliability.A wave threshold analysis suggests a sufficient reliability only off the coast, with a substantial decrease for low wave heights.  相似文献