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《Geotectonica Et Metallogenia》 1984-02
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A NEW TYPE OF DIWA REGION——ON THE GEOTEC-TONIC EVOLUTION OF THE SOUTH CHINA SEA

LIU Yixuan (South China Sea Institute of Oceanology, Academia Sinica)  
The South China Sea is a huge marginal sea at East-Asian continental margin, and a tectonic region of the transitional crust type from continental to oceanic. The formation of the South China Sea is related to the continental margin activation. It is formed by the mantle swelling and dismemberment of the continental margin tension fault. It causes the continental margin to spread out towards the ocean. It is different from Cathysian diwa regions. It was a marine diwa system of tension, and a new type of continental sea diwa regions. The characteristics of geotectonic evolution are: the geosyncline stage as the main part was in the Upper Proterozoic era, the platform stage in the Palaeozoic era. Inherited from the tectonic evolution of Cathysian diwa in a part of sea regions in the Mesozoic era, it got into the diwa stage fully in the Cenozoic era. From late Mesozoic era to Cenozoic era diwa tectonic evolution in the South China Sea may be divided into three stages: 1, From Late Cretaceous to Early Oligocene it was a stage of swelling and fracturing; 2, From Mid-Oligocene to Miocene it was a stage of fault-spreading and subsidence; 3, From Pliocene to Holoeene it was a stage of differential elevation and subsidence of fault blocks.
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