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Neotectonism of Wulong-Fuling in Wujiang drainage basin
TANG Jiang, DENG Fu—ying, LI Zhai—hui , LI Ltm-jiong
2005, 24(2):
90-93.
Crust intermittent uplifting in Wujiang river basin was responsible for three-stratum horizontal karst cavities, three-stage level surfaces, four-stage fluvial terraces and differential crust tilt-lifting brought inverted water in horizontal karst cavities and five sorts special river system such as parallel form branch, tree branch form branch, asymmetry form branch, arc form branch, shed form branch. Character of intermittent and asymmetry crust tilt-lift is showed by frequently active earthqu
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