Results 151 to 160 of about 5,526,236 (208)
Precambrian Metamorphic Basement and Sedimentary Cover of the North China Craton: A Review
Precambrian Research, 2008 The North China Craton is the largest and oldest of the three cratons in China (i.e. North China, South China and Tarim Cratons). It consists of an Archean and Paleoproterozoic metamorphic basement and overlying Mesoproterozoic unmetamorphosed ...
Guochun Zhao, Huichu Wang, Songnian Lu
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Mesozoic Basins in Eastern China and Their Bearing on the Deconstruction of the North China Craton
Journal of Asian Earth Sciences, 2012 Mesozoic basins occur widely in the Eastern Block and the neighboring area of the North China Craton, including the Bohai Bay, the Jiaolai, the Hefei and the North Yellow Sea in the north, and the Jianghan and the Subei-South Yellow Sea basins to the ...
Santosh M, Sanzhong Li, Yanhui Suo
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Metallogeny and Craton Destruction: Records From the North China Craton
Ore Geology Reviews, 2014 Abstract The link between metallogeny and craton destruction in the North China Craton (NCC) remains poorly understood, particularly the mechanisms within the interior of the craton. In this overview, we summarize the major stages in the history of formation and evolution of the NCC, the spatio-temporal distribution and types of major ore species, as
Santosh M, Sheng-Rong Li
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Destruction of the North China Craton
Science China Earth Sciences, 2012A National Science Foundation of China (NSFC) major research project, Destruction of the North China Craton (NCC), has been carried out in the past few years by Chinese scientists through an in-depth and systematic observations, experiments and theoretical analyses, with an emphasis on the spatio-temporal distribution of the NCC destruction, the ...
RiXiang Zhu +5 more
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Amalgamation of the North China Craton: Key Issues and Discussion
Precambrian Research, 2012 Abstract Geological and geophysical data indicate that the Precambrian basement of the North China Craton (NCC) formed by amalgamation of a number of micro-continental blocks. The number of blocks, when they existed and how they came together are controversial, and in particular the following issues are disputed: (1) the timing of collisional event(s)
Sanzhong Li +2 more
exaly +6 more sources
Timing of destruction of the North China Craton
Lithos, 2012Abstract The North China Craton (NCC) is the typical example of destruction of an ancient craton. However, the destruction mechanism and geodynamic controlling factors still remain enigmatic due to controversy on the timing of destruction, which is the key to understanding the destruction processes.
Ri-Xiang Zhu, Jin-Hui Yang, Fu-Yuan Wu
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Delamination and destruction of the North China Craton
Science Bulletin, 2009This article presents an overview on recent developments in studies of chemical and physical processes of lithospheric delamination with respect to destruction of the North China Craton. It is emphasized that the pyroxenite source resulting from interaction between eclogite-derived melt and peridotite is a direct consequence of delamination.
Shan Gao +3 more
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On- and off- the North China Craton
Ofioliti, 1999Geophysical data indicates that the lithosphere beneath the North China Craton (NCC) is ca 80 km thick and relatively 'hot' (Teng et al., 1983). Although this is contrary to what one might deduce from the presence of Archaean crustal rocks (ca 2.5-3.0 Ga) and Ordovician diamondiferous kimberlites (Ma and Wu, 1981), it is consistent with the information
Menzies, M. A. +4 more
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