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[null,"1.","Record Nr.",null,"UNINA9910830528303321"]
[null,null,"Titolo",null,"Himalaya : Dynamics of a Giant, Tectonic Units and Structure of the Himalaya / / edited by Rodolphe Cattin and Jean-Luc Epard"]
[null,null,"Pubbl/distr/stampa",null,"London, England : , : ISTE Ltd and John Wiley & Sons, Inc., , [2023]"]
[{"$nulls":4},"©2023"]
[null,null,"ISBN",null,"1-394-22862-7"]
[{"$nulls":4},"1-394-22859-7"]
[null,null,"Edizione",null,"[First edition.]"]
[null,null,"Descrizione fisica",null,"1 online resource (270 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. Tethyan Himalayan Sequence -- Chapter 1. Magmatism in the Kohistan-Ladakh Paleo-arc: Building Continental Crust During the India-Eurasia Convergence -- 1.1. Introduction -- 1.2. Geological setting of the Kohistan-Ladakh arc -- 1.3.Main geological contacts -- 1.3.1. The Shyok Suture Zone -- 1.3.2. The Indus Suture Zone -- 1.4. Reconstruction of the arc structure and evolution -- 1.4.1.SouthernPlutonicComplex -- 1.4.2.ChilasComplex -- 1.4.3. Gilgit Complex and Kohistan Batholith -- 1.4.4. Ladakh Batholith -- 1.5. Geochemistry and magmatic evolution of Kohistan-Ladakh magmas -- 1.5.1. Inferences for juvenile continental crust construction -- 1.5.2. Isotopic composition, inferences on the mantle source and crustal assimilation, and implications for the timing of collisions -- 1.6. Tectonic reconstructions of Kohistan-Ladakh arc evolution -- 1.6.1. Scenario 1: south-dipping subduction zone -- 1.6.2. Scenario 2: north-dipping subduction zone -- 1.7.Conclusion -- 1.8.References -- Chapter 2. Suture Zone -- 2.1. Introduction -- 2.2.General geologicaldescriptionof the ITSZ -- 2.3. The Indus suture zone of the Eastern Ladakh, the Nidar zone -- 2.3.1. The Indus group sediments -- 2.3.2. The Nidar ophiolite -- 2.3.3. The accretionary wedge or oceanic mélange -- 2.4.Conclusion -- 2.5.References -- Chapter 3. Geological Evolution of the Tethys Himalaya -- 3.1. Introduction -- 3.2.The stratigraphyof theTethysHimalaya -- 3.2.1.The pre-Tethyanhistory -- 3.2.2."]
[{"$nulls":4},"TheNeotethyanrift stage -- 3.2.3.TheNeotethyandrift stage -- 3.2.4. The Paleocene-Eocene collision stage -- 3.3.Deformationof theTethysHimalaya -- 3.3.1.Deformation and metamorphismof the Tethys Himalaya in Dolpo (WesternNepal)."]
[{"$nulls":4},"3.3.2. Deformation and metamorphism of the Tethys Himalaya inLadakh(NWIndia) -- 3.4.Conclusion -- 3.5.References -- Part 2. Greater Himalayan Crystalline Complex -- Chapter 4. High-Pressure and Ultra-High-Pressure Units in the Himalaya -- 4.1. Introduction -- 4.2. High pressure rocks in the suture zone (witnesses of the oceanic subduction) -- 4.2.1. The Shapi-Shergol blueschists (Ladakh) -- 4.2.2.TheShanglaBlueschists (Pakistan) -- 4.2.3.TheSangsangBlueschist -- 4.2.4. The Indo-Burmese Blueschists -- 4.3. Continental high-pressure (HP) to ultra-high-pressure (UHP) metamorphism of the Indian margin (continental subduction) located next to the Indus Tsangpo Suture Zone -- 4.3.1.TheKaghanunit -- 4.3.2.TheTsoMorariUHPunit -- 4.3.3. Other HP metamorphosed unit south of suture zone in the Indian continentalmargin -- 4.4. Oligocene-Miocene high-pressure, high-temperature metamorphism eclogite with granulite overprint far from the suture zone -- 4.5.Conclusion -- 4.6.References -- Chapter 5. The Greater Himalayan Sequence - Tectonic, Petrographic and Kinematic Evolution of the Metamorphic Core Zone of the Himalayan Orogeny -- 5.1. Introduction -- 5.2. Tectono-metamorphic evolution of the GHS in the central part of the Himalaya inNepal -- 5.3. Tectono-metamorphic evolution of the GHS in the north-western part of the Indian Himalaya in Himachal Pradesh and Ladakh -- 5.3.1. Metamorphism and deformation in the High Himalayan Crystalline Zone of Zanskar -- 5.3.2. Timing of crustal shortening and metamorphism along the Miyar ShearZone -- 5.3.3. Kinematic and tectonothermal evolution of the High Himalayan Crystalline Zone of Zanskar -- 5.4.Conclusion -- 5.5.References -- Chapter 6. Oligo-Miocene Exhumation of the Metamorphic Core Zone of the Himalaya Across the Range -- 6.1. Introduction -- 6.2.CentralHimalaya -- 6.3.NorthWest India -- 6.4.Conclusion."]
[{"$nulls":4},"6.5.References -- Part 3. Lesser and Sub Himalayan Sequence -- Chapter 7. Lithostratigraphy, Petrography and Metamorphism of the Lesser Himalayan Sequence -- 7.1. Introduction -- 7.2.Lithostratigraphyand petrography -- 7.2.1.Lower-LHS -- 7.2.2.Upper-LHS -- 7.2.3.Meta-igneous rocks -- 7.2.4. Along-strike variation in the LHS lithostratigraphy -- 7.3.Metamorphism -- 7.3.1.Lower-LHS -- 7.3.2.Upper-LHS -- 7.3.3.Tectonic implications -- 7.4.Conclusion -- 7.5.References -- Chapter 8. Sedimentary and Structural Evolution of the Himalayan Foreland Basin -- 8.1. Introduction -- 8.2. Overall geometry of the outer Himalayan domain -- 8.2.1.Forelandbasin geometry -- 8.2.2. Incorporation of the foreland basin into the range: a typical thin-skinnedthrust belt structure -- 8.3.Themain forelandsediments features -- 8.3.1. Present-day foothill sediments and morphology -- 8.3.2. Sedimentary facies of the Neogene Siwalik foreland basin deposits -- 8.3.3.Evolutionof sources -- 8.3.4. Evolution of environmental conditions -- 8.4. Evolution of the outer Himalayan domain: geodynamics and external processes control -- 8.4.1. Critical tectonic wedge, tectonic and surface processes velocity -- 8.4.2. Processes controlling the evolution of the foreland basin -- 8.5.Conclusion -- 8.6.References -- Conclusion -- List of Authors -- Index -- Summaries of other volumes -- EULA."]
[null,null,null,"Sommario/riassunto","The Himalaya is well known as the largest and highest mountain belt on Earth. Advances in geoscience over the past few decades have revealed a complex picture of the dynamics of this giant, opening up questions about the initial stages of Himalayan building, lateral variations in its "]
[{"$nulls":4},"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."]