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- W2384598762 abstract "The basement of the Qiangtang basin is composed of a Proterozoic metamorphic series． It has a double-layered structure． Its lower part is crystalline “hard basement” and its upper part is metamorphosed “soft basement”． Tectonically， it is characterized by one uplift sandwiched by two depressions and the presence of fault rises and fault hollows． The cover of the basin consists of Middle Devonian to Tertiary strata． In the cover， deformation is strong and there occur several sets of folds and faults． In plan view the deformation displays distinct orientation， zonation and equidistant character in section it shows differentiation and disharmony． The main deformation stage of the basin is the Indosinian-Yanshanian．" @default.
- W2384598762 created "2016-06-24" @default.
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- W2384598762 date "2001-01-01" @default.
- W2384598762 modified "2023-09-23" @default.
- W2384598762 title "Tectonic characteristics and evolution of the Qiangtang basin" @default.
- W2384598762 hasPublicationYear "2001" @default.
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