CHARACTERISTICS OF P-WAVE VELOCITY AND SEISMIC REFLECTION OF THE SEDIMENTARY LAYER IN THE SOUTH YELLOW SEA
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摘要: 南黄海为新生代、中生代与古生代叠合盆地,发育了新生代-中生代碎屑岩地层和早中生代-古生代海相碳酸盐岩地层,部分夹碎屑岩地层。在对测井资料和苏北盆地的相关资料归纳分析的基础上,总结了南黄海沉积层的纵波速度特征,标定了地震反射界面和地震反射层序。Abstract: As a superimposed sedimentary basin,the south Yellow Sea Basin contains well developed clastic deposits of Cenozoic to Mesozoic and marine carbonate sediments of early Mesozoic to Paleozoic with interbedded clastic deposits.Based on the logging data with reference to the related data from the north Jiangsu basin,we summarized in this paper the p-wave velocity characteristics of sedimentary sequence in the south Yellow Sea and calibrated the seismic reflection interfaces and sequences.
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Key words:
- south Yellow Sea /
- p-wave velocity /
- reflection sequence
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