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- W2365914840 abstract "The area studied is characterized by the southward polyleveled thrusting and decoupling in the upper crust. Evidences show that thin-skinned tectonic wedge, decreasing toward south in thickness, is constituted by the Liulin, Hongqing, Dahongshan thrusts and deeplevel decoupling in this area. It is estimated that the displacement of the Liulin sheets is 107 km or so. The thrust system propagated in a piggy-back fashion. This area exhibits a com- pllenied thrusting framework, as it is cut by several high-angle faults extending parallel to the mountain building belt. The finalized period of tectonic framework is the Yanshanian period." @default.
- W2365914840 created "2016-06-24" @default.
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- W2365914840 date "1995-01-01" @default.
- W2365914840 modified "2023-09-26" @default.
- W2365914840 title "NAPPE STRUCTURAL FRAMEWORK AND TECTONIC EVOLUTION OF SUIZHOU AREA OF HUBAI PROVINCE" @default.
- W2365914840 hasPublicationYear "1995" @default.
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