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《Chinese Journal of Geophysics》 1983-05
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ON THE STRUCTURAL FEATURE AND THE OCEANIZATION IN THE NORTH PART OF SOUTH CHINA SEA

PEI DING(Aero-geophysical and Aero-geological Division, Ministry of Geology and Mineral Resources)  
1. Both sea-floor spreading and oceanization may lead to the formation of oceanic crust. The transformation of continental crust to transitional crust is necessarily effected through the process of oceanization.2. In the deep basins within the surveyed area, the aeromagnetie anomaly zones are very similar to the symmetric linear magnetic anomaly stripes formed by sea-floor spreading.3. In the rift valley north of the Xisha Islands and in the Yingge Sea as well as zhu-1 and zhu-2 downwarps rift-type fault basins, upper mantle materials similar to oceanic crust in composition usually formed eruptions through deep fractures or were emplaced in the upper part of some extent and thus belongs to transitional type of crust. The Mohorovicic boundary surface under the submarine rift to north of Xisha Islands is about 10 km higher than that of its surrounding areas to the north and south.4. In the northern part of South China Sea, some polycentered micro-spreading and oceanization of crust have occurred.
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