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- W2353642941 abstract "The geotectonic basis of China is founded on the T-joint of the structural belts ofthe tethys and the Circum-Pacific,of which the subbelts are interwoven to form a tri-angular network (Fig.1).This is why there can hardly be found any such geotectonicunits as the Russian,the Laurantian,the African,the Australian,and the Brazilian plat-forms.The so-called Sino-Korean platform and the Tarimian platform are reallyrelatively more prominant median massives in the network of the interwoven tectonicbelts.On such a geotectonic background,the crustal segment of China should be ine-vitably broken into relatively small pieces,that is determinative of the activity of theirmovements,the complexity of their structural developments,the scattering of the distribu-tion of igneous formations,and the richness and veriability of ore deposits,in short thatmakes the crustal segment of China non-platform in character." @default.
- W2353642941 created "2016-06-24" @default.
- W2353642941 creator A5015445866 @default.
- W2353642941 date "1966-01-01" @default.
- W2353642941 modified "2023-09-23" @default.
- W2353642941 title "THE BASIC GEOTECTONIC CHARACTERS OF CHINA AND THE MECHANISM OF THE FORMATION OF MOSAIC STRUCTURES" @default.
- W2353642941 hasPublicationYear "1966" @default.
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