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冲绳海槽中部无井区速度场建立及应用
陈若瑜1,2, 李 琦1, 胡俊杰1, 邵 威1, 葛东升1, 蔡 峰2, 闫桂京2, 李 清2
1.中国地质大学 海洋学院;2.青岛海洋地质研究所
摘要:
速度场的建立是冲绳海槽中部深入研究所必需的技术资料。作者选取冲绳海槽中部无井深水区二维地震数据, 以数据处理过程中的叠加速度数据为原始速度, 通过建立双层模型和异常速度识别剔除, 采用Dix 公式方法进行速度转换和沿层速度插值, 建立研究区速度场。从区域速度场问题建立宏观概念, 为冲绳海槽中部提供丰富可靠的速度资料, 变速成图得到的构造图件与地质认识相一致, 实现了由地震资料反映海底构造等地质信息的目的。
关键词:  冲绳海槽中部  无井深水区  速度场  Dix 公式法
DOI:10.11759/hykx20140529001
分类号:
基金项目:国家自然科学基金资助项目(41306062); 国土资源部天然气水合物重点实验室开放基金资助项目(SHW[2014]-DX-02, [2014]-DX-04); 国家海洋局海底科学重点实验室基金资助项目(KLSG1202)
Establish and application of the velocity field in the middle Okinawa Trough of Non-well area
Abstract:
Establishing the velocity field is necessary for in-depth study of the central Okinawa Trough. In this paper, two-dimensional seismic data of the no-well deep-water area in the middle Okinawa Trough were selected for the study. The stacking velocity data during processing of seismic data were obtained as the raw velocity data. By establishing the layer model and exception speed identification removal, using the Dix formula approach speed conversion and interpolation along the velocity, the velocity field was established in the study area. The establishment of the velocity field from the macro-regional concept, provides speed information for the central Okinawa trough. By completing the variable velocity mapping, it uses geological information to reflect the subsea construction.
Key words:  the middle Okinawa Trough  non well deep-water  the velocity field  DIX formula method
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