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[null,"1.","Record Nr.",null,"UNINA9910130751703321"]
[null,null,"Titolo",null,"Dynamics and exchanges in estuaries and the coastal zone"]
[null,null,"Pubbl/distr/stampa",null,"[Place of publication not identified], : American Geophysical Union, 1992"]
[null,null,"ISBN",null,"1-118-66527-9"]
[null,null,"Collana",null,"Coastal and estuarine studies  Dynamics and exchanges in estuaries and the coastal zone"]
[null,null,"Disciplina",null,"551.46/09"]
[null,null,"Soggetti",null,"Estuarine oceanography - Congresses"]
[{"$nulls":4},"Coasts - Congresses"]
[{"$nulls":4},"Earth & Environmental Sciences"]
[{"$nulls":4},"Marine Science"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Note generali","Bibliographic Level Mode of Issuance: Monograph"]
[null,"2.","Record Nr.",null,"UNINA9910418019803321"]
[null,null,"Autore",null,"Adam Michel"]
[null,null,"Titolo",null,"Le Temps de la mémoire : le flux, la rupture, l’empreinte"]
[null,null,"Pubbl/distr/stampa",null,"Pessac, : Presses Universitaires de Bordeaux, 2020"]
[null,null,"ISBN",null,"979-1-03-000538-7"]
[null,null,"Descrizione fisica",null,"1 online resource (494 p.)"]
[null,null,"Soggetti",null,"Literature (General)"]
[{"$nulls":4},"fiction"]
[{"$nulls":4},"transgression"]
[{"$nulls":4},"sédiment"]
[{"$nulls":4},"écriture de soi"]
[{"$nulls":4},"lieu de mémoire"]
[{"$nulls":4},"sensation"]
[{"$nulls":4},"flux"]
[{"$nulls":4},"mémoire antique"]
[{"$nulls":4},"temps perdu"]
[{"$nulls":4},"souvenir traumatique"]
[{"$nulls":4},"mémoire"]
[null,null,"Lingua di pubblicazione",null,"Francese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Sommario/riassunto","L’expérience essentielle du rapport au Temps est un champ particulièrement riche sur le plan imaginaire et symbolique. Comment cerner ce rapport au temps ? Comment mettre en mot les bribes, les sédiments, les quêtes de la mémoire ? Les contributions rassemblées dans ce volume, s’attachant à la longue durée, de l’antiquité à l’époque contemporaine, témoignent d’une heureuse confluence des interrogations : la mémoire veut capturer le flux du temps révolu, elle affronte les ruptures du fil temporel, elle occulte ou révèle le traumatisme, elle déchiffre l’empreinte, le vestige dont il importe de retrouve j’origine et le sens. Dans cette entreprise complexe, l’équivoque s’associe à l’oubli, la voix doit assurer une transmission incertaine ; l’histoire et la fiction veulent, chacune à sa manière, faire surgir l’architecture du temps passé, recomposer les lieux et les "]
[{"$nulls":4},"moments. Le discours de mémoire est une texture dont l’écriture littéraire, tout particulièrement, suggère les déchirements.  La mémoire serait-elle un « sixième sens à elle seule » (J.Y. Tadié) ? La diversité des contributions dans ce volume est fondée sur la pluridisciplinarité des approches et des interprétations. La symbolique individuelle ou collective, les témoignages communautaires ou personnels, les croyances enracinées dans les patrimoines proposent leurs énigmes, secrets et révélations, qui concernent aussi bien l’anthropologue que le psychanalyste, les historiens et les spécialistes de la littérature et de l’art. Le Moi, gardien inquiet de sa propre-mémoire, rejoint alors, en une communauté riche de sens, les passeurs de mémoire qui usent de leur voix singulière pour tisser le rapport au temps collectif. La traque du temps passé, l’inquiétude de la quête, l’incertitude du devenir au miroir de la mémoire, contribuent à la constitution des identités, dans nos sociétés comme dans les autres cultures."]
[null,"3.","Record Nr.",null,"UNINA9910735567003321"]
[null,null,"Titolo",null,"Himalaya, dynamics of a giant 1 : Geodynamic setting of the Himalayan range / / Rodolphe Cattin, Jean-Luc Epard"]
[null,null,"Pubbl/distr/stampa",null,"London, England : , : ISTE Ltd and John Wiley & Sons, Inc., , [2023]"]
[{"$nulls":4},"©2023"]
[null,null,"ISBN",null,"1-394-22858-9"]
[{"$nulls":4},"1-394-22856-2"]
[null,null,"Edizione",null,"[First edition.]"]
[null,null,"Descrizione fisica",null,"1 online resource (301 pages)"]
[null,null,"Disciplina",null,"915.49604"]
[null,null,"Soggetti",null,"Himalaya Mountains Region Description and travel"]
[null,null,"Lingua di pubblicazione",null,"Inglese"]
[null,null,"Formato",null,"Materiale a stampa"]
[null,null,null,"Livello bibliografico","Monografia"]
[null,null,null,"Nota di bibliografia","Includes bibliographical references and index."]
[null,null,"Nota di contenuto",null,"Cover -- Title Page -- Copyright Page -- Contents -- Tributes -- Foreword -- Preface. From Research to Education: The Example of the Seismology at School in Nepal Program -- Part 1. Tectonic Framework of the Himalaya and Tibet -- Chapter 1. Plate Reconstructions and Mantle Dynamics Leading to the India-Asia Collision -- 1.1. Introduction -- 1.2. The India-Asia convergence and the age of the collision -- 1.2.1.The India-Asia convergence -- 1.2.2. The age of the India-Asia collision -- 1.3. Plate collision configurations -- 1.3.1. Reconstructing lost continental margins -- 1.3.2. Alternative collision configurations -- 1.4. Reconstruction of the Neotethys Ocean closure dynamic -- 1.4.1. Number of subduction accommodating the Neotethys closure -- 1.4.2. Location of the Intraoceanic subduction zone and associated arc -- 1.4.3. Driving forces of the India-Asia convergence during Neotethys closure -- 1.5.Conclusion -- 1.6.References -- Chapter 2. Building the Tibetan Plateau During the Collision Between the India and Asia Plates -- 2.1. Introduction -- 2.2.Present-dayTibetan crustal deformation -- 2.2.1. GPS velocity field and focal mechanisms in Tibet -- 2.2.2. Surface motions and deformation due to Indian indentation -- 2.3. Tibetan lithospheric mantle subduction during collision -- 2.3.1. Imaging ongoing subduction beneath Tibet -- 2.3.2. Imaging subduction of lithospheric Tibetan mantle during the collision -- 2.3.3. Volcanism in Tibet showing the subduction of lithospheric Asian mantle during the early collision -- 2.4. Modeling the Tibetan plateau formation during the indentation of the Indiancontinent intoAsia -- 2.4.1. Analogue modeling of the "]
[{"$nulls":4},"Tibetan lithosphere subduction duringthe indentationof India -- 2.4.2. Numerical modeling of Asian thickening and extrusion during the subduction of a continental-oceanic plate -- 2.5.Conclusion."]
[{"$nulls":4},"2.6.References -- Chapter 3. The Major Thrust Faults and Shear Zones -- 3.1. Introduction -- 3.2.Some basic concepts -- 3.3.Main faults andshear zones -- 3.3.1. South Tibetan detachment system (STDS) -- 3.3.2.MainCentral thrust (MCT) -- 3.3.3. Main Boundary thrust (MBT) -- 3.3.4.MainFrontal thrust (MFT) -- 3.3.5. Main Himalayan thrust (MHT), continental megathrust -- 3.4.Tectonicmodels -- 3.4.1. Fold-and-thrust belt versus channel flow -- 3.4.2.Coeval slip along theSTDSand theMCT -- 3.5.Conclusion -- 3.6.References -- Part 2. Along Strike Variations -- Chapter 4. Seismological Imaging and Current Seismicity of the Himalayan Arc -- 4.1. Introduction -- 4.2. Imagingby elasticwaves -- 4.2.1.Active seismics -- 4.2.2.Passive seismics -- 4.2.3. Tomographic imaging for bulk properties -- 4.2.4.Wave reflections and conversions for interfaces -- 4.3. Exploring the Central Himalaya along cross-sections -- 4.3.1.Field experiments -- 4.3.2. Main interfaces -- 4.3.3.Where do subducted plates go? -- 4.4.Lateral variations -- 4.4.1. Lateral ramps on the MHT, along-arcMoho variations -- 4.4.2. Segmentation of the India plate lithosphere -- 4.4.3.Thewestern andeastern syntaxes -- 4.5.Current seismicity of theHimalaya -- 4.5.1. Earthquake detection, location and activity -- 4.5.2. Seismicity of the Himalaya: an incomplete patchwork -- 4.5.3.Seismicity of theHimalaya:main features -- 4.6.Conclusion -- 4.7.References -- Chapter 5. Gravity Observations and Models Along the Himalayan Arc -- 5.1. Introduction -- 5.2. Methods -- 5.2.1. Measurements -- 5.2.2.Corrections -- 5.2.3.Anomalies -- 5.3. Isostasy -- 5.3.1.Local compensation -- 5.3.2.Regional compensation -- 5.3.3.Effectiveelastic thickness -- 5.4.Flexure of the Indianplate -- 5.4.1. Gravity anomaly across the Himalayan belt -- 5.4.2. Along-strike variation between Nepal and Bhutan -- 5.5. Satellite data contribution."]
[{"$nulls":4},"5.5.1.Gravitymeasurements fromspace -- 5.5.2. Towards a three-dimensional image -- 5.6.Conclusion -- 5.7.References -- Chapter 6. Topographic and Thermochronologic Constraints on the Himalayan Décollement Geometry -- 6.1. Introduction -- 6.2. Methods -- 6.2.1. Quantitative geomorphic analysis -- 6.2.2. Measures of erosion at different timescales: cosmogenic nuclides and thermochronology -- 6.2.3. From exhumation to kinematics: thermo-kinematic models -- 6.3.Regional case studies -- 6.3.1.CentralHimalaya-Nepal -- 6.4.Discussion -- 6.4.1. Constraints on MHT geometry and kinematics at different timescales -- 6.4.2.Nature and evolutionof rampson theMHT -- 6.4.3. Evidence for out-of-sequence thrusting? -- 6.4.4.Lateral segmentationof theMHT -- 6.5.Conclusion -- 6.6.References -- Part 3. Focus -- Chapter 7. Application of Near-surface Geophysical Methods for Imaging Active Faults in the Himalaya -- 7.1. Introduction -- 7.2. Near-surface geophysics -- 7.2.1. Geophysical methods for fault mapping -- 7.2.2. Case study data and inversion technique -- 7.3. Geophysical results of case study from south Bhutan -- 7.3.1.Electrical resistivity tomography -- 7.3.2.Seismic tomography -- 7.3.3.Micro-gravity -- 7.4. Implications of near-surface geophysical findings -- 7.4.1.Subsurface imaging -- 7.4.2.Overthrustingslip rate assessment -- 7.4.3. Deformation at the topographic front -- 7.5.Conclusion -- 7.6.References -- Chapter 8. Overview of Hydrothermal Systems in the Nepal Himalaya -- 8.1. Introduction -- 8.2. Measurement methods -- 8.2.1.Explorationapproach -- 8.2.2.Thermal springwatermeasurements -- 8.2.3. CO2 flux and radonfluxmeasurements -- 8.2.4. Carbon content and isotopic composition measurements -- 8.3. Summary of results at the hydrothermal sites in the Nepal Himalaya -- 8.3.1. "]
[{"$nulls":4},"Overview of hydrothermal sites in Far-Western Nepal."]
[{"$nulls":4},"8.3.2. Overview of hydrothermal sites in Mid-Western Nepal -- 8.3.3. Overview of hydrothermal sites in Western Nepal -- 8.3.4. Overview of hydrothermal sites in Central Nepal -- 8.3.5. Overview of hydrothermal sites in Eastern Nepal -- 8.3.6. Overview of hydrothermal sites in the MFT zone -- 8.4.Conclusion -- 8.5.References -- Conclusion -- Rodolphe CATTIN and Jean-Luc EPARD of Authors -- Index -- Summaries of other volumes -- EULA."]
[null,null,null,"Sommario/riassunto","The Himalaya is well known as the largest and highest mountain belt on Earth. Advances in geoscience over the past few decades have revealed a complex picture of the dynamics of this giant, opening up questions about the initial stages of Himalayan building, lateral variations in its structures, variations in tectonic forcing, tectonic-climate coupling and assessments of the natural hazards affecting this area. In this three-volume book, we present the current knowledge on the building and present-day behavior of the Himalayan range. The objective is not to be exhaustive, but to provide some key elements used by researchers to unravel the many processes acting in the Himalayan dynamics. Mountain environments are at the forefront of climate change with glacier retreat, landslides, flash floods and water availability. Understanding the delicate balance that controls the dynamics of the Himalayan giant is now, more than ever, a major challenge for the scientific community."]