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- W2354068375 abstract "Several nappes have been found in the late Paleozoic and Mesozoic coal-bearing basins in southeastern Hunail.It is known that the nappes formed in the maximum-and residual-mobility periods of diwa development during the early Yanshaninn and Himalayan orogenies.Their features and development are markedly different form those of Alpine-type nappe found in geosynclinal-folded belts.It follows that the nappes are a general structural feature characteristic of a diwa region.The author proposes to call them diwa-type nappes.Elucidation of the basic features of such a structural featufe,the tectonic setting of its occurrence and the mechanism of its formation is of important significance for the study of tectonic structures and exploration for minerals." @default.
- W2354068375 created "2016-06-24" @default.
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- W2354068375 date "1987-01-01" @default.
- W2354068375 modified "2023-09-28" @default.
- W2354068375 title "MESO-CENOZOIC NAPPES IN SOUTHEASTERN HUNAN AND THEIR SIGNIFICANCE" @default.
- W2354068375 hasPublicationYear "1987" @default.
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