Tectonics and Geodynamics of South China: an introductory note
Résumé
Highlights:
• The Neoproterozoic Jiangnan collision of Cathaysia and Yangtze is responsible for the formation of the South China Block (SCB)
• During the Early Paleozoic, the SCB was welded to the North China block along the Qinling belt, and also experienced an intracontinental orogeny that partly reworked the Jiangnan belt.
• During the Middle Triassic, the SCB was welded to Indochina, the Qinling belt was reworked by N-directed intracontinental subduction.
• The Xuefengshan belt is also a Middle Triassic intracontinental orogen.
| Origine | Fichiers produits par l'(les) auteur(s) |
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