LEADER 03068nam 2200673 a 450 001 9910777873803321 005 20200520144314.0 010 $a1-383-04143-1 010 $a1-280-84110-9 010 $a0-19-153371-8 010 $a1-4294-5939-5 035 $a(CKB)1000000000471477 035 $a(EBL)415151 035 $a(OCoLC)476240435 035 $a(SSID)ssj0000120152 035 $a(PQKBManifestationID)11141034 035 $a(PQKBTitleCode)TC0000120152 035 $a(PQKBWorkID)10080913 035 $a(PQKB)11345424 035 $a(Au-PeEL)EBL415151 035 $a(CaPaEBR)ebr10271503 035 $a(CaONFJC)MIL84110 035 $a(Au-PeEL)EBL7033722 035 $a(MiAaPQ)EBC415151 035 $a(EXLCZ)991000000000471477 100 $a20060823d2006 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 10$aCharles Dickens and his performing selves$b[electronic resource] $eDickens and the public readings /$fMalcolm Andrews 210 $aOxford ;$aNew York $cOxford University Press$d2006 215 $a1 online resource (346 p.) 300 $aDescription based upon print version of record. 311 $a0-19-923620-8 311 $a0-19-927069-4 320 $aIncludes bibliographical references and index. 327 $aPreface and Acknowledgements; Contents; List of Illustrations; A Premiere: New York, December 1867; 1. A Community of Readers; 2. Reading, Reciting, Acting; 3. Impersonation; 4. Celebrity on Tour; 5. Performance; 6. A 'New Expression of the Meaning of my Books'; Finale: London, March 1870; Appendix: Schedule of the Public Readings; Abbreviations; Notes; Index 330 $aCharles Dickens's public readings have not had the attention they deserve; and yet Dickens put as much effort into perfecting his performances as he did with his novels. These performances were sensational events and won Dickens thousands of new admirers. This book tells that story and brings the events alive, with more detail than ever before. - ;Charles Dickens had three professional careers: novelist, journalist and public Reader. That third career has seldom been given the serious attention it deserved. For the last 12 years of his life he toured Britain and America giving 2-hour readings 606 $aOral interpretation of fiction$xHistory$y19th century 606 $aOral reading$xHistory$y19th century 606 $aPerforming arts$zGreat Britain$xHistory$y19th century 606 $aPerforming arts in literature 606 $aStage adaptations 615 0$aOral interpretation of fiction$xHistory 615 0$aOral reading$xHistory 615 0$aPerforming arts$xHistory 615 0$aPerforming arts in literature. 615 0$aStage adaptations. 676 $a823/.8 700 $aAndrews$b Malcolm$0460491 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910777873803321 996 $aCharles Dickens and his performing selves$91125389 997 $aUNINA LEADER 07629nam 2200493 450 001 9910830528303321 005 20230807193832.0 010 $a1-394-22862-7 010 $a1-394-22859-7 035 $a(MiAaPQ)EBC7269054 035 $a(Au-PeEL)EBL7269054 035 $a(BIP)093484536 035 $a(EXLCZ)9927531924500041 100 $a20230807d2023 uy 0 101 0 $aeng 135 $aurcnu|||||||| 181 $ctxt$2rdacontent 182 $cc$2rdamedia 183 $acr$2rdacarrier 200 00$aHimalaya $eDynamics of a Giant, Tectonic Units and Structure of the Himalaya /$fedited by Rodolphe Cattin and Jean-Luc Epard 205 $aFirst edition. 210 1$aLondon, England :$cISTE Ltd and John Wiley & Sons, Inc.,$d[2023] 210 4$d©2023 215 $a1 online resource (270 pages) 311 08$aPrint version: Cattin, Rodolphe Himalaya: Dynamics of a Giant, Tectonic Units and Structure of the Himalaya Newark : John Wiley & Sons, Incorporated,c2023 9781789451306 320 $aIncludes bibliographical references and index. 327 $aCover -- 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.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). 327 $a3.3.2. 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. 327 $a6.5.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. 330 8 $aThe 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. 607 $aHimalaya Mountains Region$xDescription and travel 610 $aGeophysics 610 $aGeology 610 $aScience 676 $a915.49604 702 $aCattin$b Rodolphe 702 $aEpard$b Jean-Luc 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910830528303321 996 $aHimalaya$92584298 997 $aUNINA