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 inJournal of earth science (Wuhan, China) Vol. 23; no. 3; pp. 277 - 284
Main Authors Kusky, Timothy M., Zhai, Mingguo
Format Journal Article
LanguageEnglish
Published China University of Geosciences China University of Geosciences 01.06.2012
Springer Nature B.V
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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.
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.
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ISSN:1674-487X
1867-111X
DOI:10.1007/s12583-012-0253-6