中国海洋湖沼学报(英文版)
中國海洋湖沼學報(英文版)
중국해양호소학보(영문판)
Chinese Journal of OCEANOLOGY and LIMNOLOGY
2003年
4期
377-388
,共12页
吴时国%刘展%王万银%郭军华%T.Lüdmann%H.K.Wong
吳時國%劉展%王萬銀%郭軍華%T.Lüdmann%H.K.Wong
오시국%류전%왕만은%곽군화%T.Lüdmann%H.K.Wong
Late Cenozoic tectonic movement%seismic stratigraphy%plate collision%South China Sea
Dongsha Island and the adjacent sea area locate at the northern continental margin of the South China Sea (SCS), and is connected to the east by the Manila Trench. Analyses of seismic stratigraphy and gravity, magnetic and drilling wells data led to the discovery of three post-fault sequences (V, VI, VII). Extensive tectonic uplift, magma activity and erosion occurred in Dongsha Island and the adjacent area, where most of the faults in the northeastern SCS were still active during Pliocene and Quaternary. Two groups of faults trending NEE and NW were developed during Late Cenozoic. We conclude that three important tectonic movements, especially Dongsha movement (4.4-5.2 Ma) and Liuhua movement (1.4-1.89 Ma), controlled the structural framework in the Dongsha rise; whose deformation in the east is stronger than that in the west and whose stress field variation suggests that the tectonic uplift in the study area contributed to magmato-tectonic events correlated to the main collision phases between the East China and Taiwan 5-3 and 3-0 Ma ago.