Late Palaeozoic–Early Mesozoic geological features of South China: Response to the Indosinian collision events in Southeast Asia

Liangshu S. Shu (1) , Michel Faure (2) , Bo Wang (1) , Xinmin Zhou (1) , Biao Song (3)

1 Department of Earth Sciences [Nanjing]
2 ISTO - Institut des Sciences de la Terre d'Orléans
3 Center of Iron-Probe in Beijing

This paper provides some new evidences on stratigraphic sequence, zircon SHRIMP dating from ophiolite, granitoids, and fold-and-thrust tectonic styles in the South China Block (SCB). Stratigraphic studies suggest that the eastern and central parts of the SCB show a SW-dipping palaeoslope framework during the Late Palaeozoic–Early Mesozoic. These areas were not in a deep-sea environment, but in a shallow-sea or littoral one. Coeval volcanic rocks are missing. Deep-water deposits and submarine volcanism only took place in the western part of the SCB. The three ophiolitic mélanges of the eastern SCB formed in the Neoproterozoic, but not in the Permian or the Triassic. The sedimentary rocks associated with the Neoproterozoic oceanic relics contain abundant Proterozoic acritarchs, but no radiolarians. The Early Mesozoic granitoids (235–205 Ma) belong to the post-collision peraluminous S-type granites; they are widely exposed in the central-western SCB, and rare in the eastern SCB. The fold-and-thrust belt developed in the eastern SCB shows a top-to-the-south displacement, whereas the Xuefengshan Belt of central SCB indicates a north- or northwest-directed shearing. The geodynamic settings of the different parts of the SCB during the Triassic are discussed.

Keywords: Stratigraphy; Deformation; Ophiolite; Granitoids; Late Palaeozoic–Early Mesozoic; Indosinian event; South China

Domains: Sciences of the Universe [physics]; Earth Sciences; Tectonics; Environmental Sciences; Global Changes

Liangshu S. Shu, Michel Faure, Bo Wang, Xinmin Zhou, Biao Song. Late Palaeozoic–Early Mesozoic geological features of South China: Response to the Indosinian collision events in Southeast Asia. Comptes Rendus Géoscience, 2008, 340, pp.151-165. ⟨insu-00202662⟩