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Geotectonic Evolution of China Softcover reprint of the original 1st ed. 1987 [Pehme köide]

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  • Formaat: Paperback / softback, 218 pages, kõrgus x laius: 235x155 mm, kaal: 367 g, X, 218 p., 1 Paperback / softback
  • Ilmumisaeg: 13-Feb-2012
  • Kirjastus: Springer-Verlag Berlin and Heidelberg GmbH & Co. K
  • ISBN-10: 3642648746
  • ISBN-13: 9783642648748
Teised raamatud teemal:
  • Formaat: Paperback / softback, 218 pages, kõrgus x laius: 235x155 mm, kaal: 367 g, X, 218 p., 1 Paperback / softback
  • Ilmumisaeg: 13-Feb-2012
  • Kirjastus: Springer-Verlag Berlin and Heidelberg GmbH & Co. K
  • ISBN-10: 3642648746
  • ISBN-13: 9783642648748
Teised raamatud teemal:
Anyone studying the geology and tectonics of China and who is not able to read Chinese will need to have a copy of this book: Ceotectonic Evolution of China and a companion copy of the Tectonic Map of China, scale 1:4000,000. Professor Huang Jiqing and his collaborators from the Institute of Geology, Chinese Academy of Geological Sciences have provided the English-speaking earth scientists with an extremely valuable tool that can be used towards understanding the geo­ b;;y of China. The introductory chapter is necessary to read prior to effective use of the material discussed in other chapters as it clearly presents the philosophy of this school of tectonics. The collaborators of the book acknowledge the important changes have been brough about by the plate tectonics theory but do not fully incorporate these ideas into their discussion. The book and map are testimony to the tremendous amount of geologic work accomplished by Chinese geologists in the past fourty years. As our Chinese collea­ gues begin to publish more English summaries such as this, it will become apparent to the rest of the world the vast amount of geologic mapping along with supportive stratigraphy and geophysics that has already been accomplished. Nearly all major non­ Chinese tracts on tectonic synthesis of the world treat China in only a cursory fashio)1 because so little is known of the area. With this text and map, future world tectonic synthesis can no longer afford to leave China out of the picture.

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I. On the Problem of Methods and Theories.- I.1 On the Method of
Historical Analysis.- I.2 On Some Theoretical Problems of Geotectonics.- II.
Subdivision of the Tectonic Cycles of China.- II.1 The Fuping Cycle.- II.2
The Wutai Cycle.- II.3 The Zhongtiao Cycle.- II.4 The Wuling Cycle.- II. 5
The Yangtze Cycle.- II. 6 The Xingkai Cycle.- II.7 The Caledonian Cycle.- II.
8 The Variscan Cycle.- II. 9 The Alpine Cycle.- III. Brief Description of the
Main Tectonic Units of China.- III.1 System of Nomenclature for Tectonic
Units.- III.2 The Sino-Korean Para platform.- III.3 The Yangtze
Paraplatform.- III.4 The Tarim Platform.- III.5 The South China Sea
Platform.- III.6 The Sayan-Ergun Géosynclinal Fold Region.- III.7 The
Tianshan-Hinggan Géosynclinal Fold Region.- III.8 The Kunlun-Qinling
Géosynclinal Fold Region.- III.9 The Yunnan-Tibet Géosynclinal Fold Region.-
III.10 The Himalayan Géosynclinal Fold Region.- III.11 The Marginal-Pacific
Géosynclinal Fold Region.- III.12 The Géosynclinal Fold Region of the Western
Pacific Island Arcs.- III.13 The Epicontinental Basins and Marginal Sea
Basins in Eastern China.- IV. The Geosynclines of China and Their Main
Characteristics.- IV.1 The Subdivision of the Geosynclines of China and Their
Development.- IV.2 The Classification of the Geosynclines of China and the
Sequence of Their Sedimentary Formations.- IV. 3 The Formation and
Transformation of the Geosynclines of China.- IV.4 The Contact Relationship
Between the Geosynclines and Platforms of China.- IV.5 The Poly cyclic
Development of the Geosynclines of China.- V. Deep Fractures and Deep-Seated
Structures in China.- V.1 The Tectonic Framework Shown by Deep Fractures in
China.- V.2 Brief Descriptions of the Main Deep Fractures in China.- V.3 The
Relationship Between TectonicFramework of the Fractures and Deep-Seated
Structures of China.- VI. The Geotectonic Evolution of China.- VI.1 The
Archean and Eo-Algonkian Megacycle (Archean-Early Proterozoic) Gradual
Formation of the Sino-Korean Para platform.- VI.2 The Neo-Algonkian Megacycle
(Late Proterozoic) the Formation of the Chinese Protoplatform.- VI. 3 The
Establishment of the Xingkai Cycle and the Disintegration of the Chinese
Protoplatform.- VI.4 The Early Neogaic Megacycle (Paleozoic) the Formation
of Pal-Asia.- VI.5 The Late Neogaic Megacycle (Mesozoic-Cenozoic) the
Formation and Development of the Marginal-Pacific Tectonic Domain and the
Tethys-Himalayan Tectonic Domain.- VI.6 The Himalayan Movement and Its
Significance in the Tectonic Development of China.- References.- Explanations
of Plates.