Early Continent Evolution of the North China Craton

Häftad, Engelska, 2024

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Beskrivning

Early Continent Evolution of the North China Craton discusses the tectono-thermal regimes of the early continental crust in the North China Craton (NCC), from the Hadean to the early Paleoproterozoic, reconstructing the evolutional framework and facilitating comprehensive understanding of the early continent evolution of the NCC. The book systematically summarizes the Neoarchean metamorphism of the NCC and discusses the implications for the tectonic models of the NCC through compiling evolutional information of the Hadean to the early Paleoproterozoic sequences in the NCC.

Researchers, academics, and students in geology (especially Precambrian Geology), geomorphology, geophysics, and geological engineering will benefit from using this book in applying tectonic models to other cratonic blocks globally, and will understand evolutional information of the largest and oldest cratonic block in China.

Completely covers all key issues and research frontiers of the early continental evolution of the North China Craton (NCC), from the Hadean to the early Paleoproterozoic
Systematically summarizes the Neoarchaean metamorphism of the NCC and discusses the implications for tectonic models
Includes discussion on controversial views on tectonic regimes of the NCC during the Archean to early Paleoproterozoic, with objective conclusions

Produktinformation

Utgivningsdatum:2024-03-28
Mått:152 x 229 x 19 mm
Vikt:530 g
Format:Häftad
Språk:Engelska
Antal sidor:328
Förlag:Elsevier Science
ISBN:9780443138898

Utforska kategorier

Geologi inom Naturvetenskap och teknik
Paleontologi inom Naturvetenskap och teknik

Mer om författaren

Professor Mingguo Zhai works in the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, University of Chinese Academy of Sciences, China and specializes in Precambrian and metamorphic geology, and petrology. His main research interests are Precambrian tectonic evolution in China; High-temperature and high-pressure metamorphiam and reconstruction of Precambrian; Ultra-high-pressure metamorphism and continental collision; Mesozoic tectonic evolution of the North China Block. Professor Peng Peng works in the China-Brazil Joint Geoscience Research Center, Institute of Geology and Geophysics, University of Chinese Academy of Sciences, China and specializes in Precambrian geology. His research interests include Precambrian tectonics, particularly the Precambrian evolution of cratons, supercontinents and the Earth system, and the comparison of the Precambrian and modern tectonics. Currently, he is an editor/associate editor of Precambrian Research, Island Arc, Analysis and Testing Technology and Instruments, Geotectonica et Metallogenia, etc. Professor Yanyan Zhou works in the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, China and specializes in Precambrian geology, Geochronology, and Geochemistry. His research interests are on Precambrian igneous rocks and the Precambrian crustal evolution of North China Craton. Professor Lei Zhao works in the State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, University of Chinese Academy of Sciences, China and specializes in Precambrian geology, Zircon Geochronology, Metamorphic Petrology, and Geochronology.

Innehållsförteckning

1. Introduction to the early continental evolution of the North China Craton (NCC)2. General generation and growth of Precambrian continental crust3. Precambrian outline of the North China Craton4. Oldest continental rocks in Hadean-Paleoarchean in the North China Craton5. Magmatic evolution and recycling for Mesoarchean continental crust of the North China craton6. Neoarchean continental evolution in the North China Craton7. Neoarchean metamorphism of the North China Craton8. Lithospheric evolution during the 2.5–2.1 Ga critical period following the Neoarchean cratonization9. The early plate tectonics: from vertical differentiation to horizontal accretion