The Neoarchean Ophiolite in the North China Craton: Early Precambrian Plate Tectonics and Scientific Debate
Archean greenstone belts and their possible inclusion of fragments of ophiolites is an im-portant research subject, since it is correlated with the nature of early oceanic crust, and can yield in-formation on the nature of early planetary lithospheres, the origin of TTG (tonalite-trondhjemite-granod...
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Published in | Journal of earth science (Wuhan, China) Vol. 23; no. 3; pp. 277 - 284 |
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Main Authors | , |
Format | Journal Article |
Language | English |
Published |
China University of Geosciences
China University of Geosciences
01.06.2012
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | Archean greenstone belts and their possible inclusion of fragments of ophiolites is an im-portant research subject, since it is correlated with the nature of early oceanic crust, and can yield in-formation on the nature of early planetary lithospheres, the origin of TTG (tonalite-trondhjemite-granodiorite) continental crust, the formation of early cratons and continents, and is related to when plate tectonics started in the Earth's evolutionary history. This article briefly reviews the North China craton's Archean ophiolite argument and proposes further studies aimed at understanding the genera- tion of greenstone belts and Archean ophiolites, and suggests some key scientific questions that remain to be answered. |
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Bibliography: | Archean, ophiolite, greenstone belt, North China craton. Timothy M Kusky,Mingguo Zhai (Three Gorges Research Center for Geo-hazards, Ministry of Education, China University of Geosciences, Wuhan 430074, China; State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China;State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China) Archean greenstone belts and their possible inclusion of fragments of ophiolites is an im-portant research subject, since it is correlated with the nature of early oceanic crust, and can yield in-formation on the nature of early planetary lithospheres, the origin of TTG (tonalite-trondhjemite-granodiorite) continental crust, the formation of early cratons and continents, and is related to when plate tectonics started in the Earth's evolutionary history. This article briefly reviews the North China craton's Archean ophiolite argument and proposes further studies aimed at understanding the genera- tion of greenstone belts and Archean ophiolites, and suggests some key scientific questions that remain to be answered. 42-1788/P SourceType-Scholarly Journals-1 ObjectType-Feature-1 content type line 14 ObjectType-Article-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 1674-487X 1867-111X |
DOI: | 10.1007/s12583-012-0253-6 |