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作 者:YANG Yan JIANG Linshun ZHANG Dong QIN Qianqing XU Lin
机构地区:[1]School of Physics and Technology, Wuhan University,Wuhan 430072, Hubei, China [2]State Key Laboratory of Information Engineering inSurveying, Mapping and Remote Sensing/Wuhan University, Wuhan430072, Hubei, China [3]Research Institute of Petroleum Exploration and Production,China National Petroleum Corporation, Beijing 100082, China
出 处:《Wuhan University Journal of Natural Sciences》2010年第6期505-509,共5页武汉大学学报(自然科学英文版)
基 金:Supported by the National Natural Science Foundation of China (69983005)
摘 要:An approach of three-dimensional seismic ray tracing is presented,which is derived from adopting two-dimensional linear traveltime interpolation(LTI).By adjusting the forward process using the partition of grid interface,and backward step by considering more directions,the new approach is suitable for the application of three-dimensional models.The calculation results show that,with the same accuracy,the improved 3-D method is much faster than the method of traditional LTI directly applied in the three-dimensional case.An approach of three-dimensional seismic ray tracing is presented,which is derived from adopting two-dimensional linear traveltime interpolation(LTI).By adjusting the forward process using the partition of grid interface,and backward step by considering more directions,the new approach is suitable for the application of three-dimensional models.The calculation results show that,with the same accuracy,the improved 3-D method is much faster than the method of traditional LTI directly applied in the three-dimensional case.
关 键 词:3-D ray tracing linear traveling interpolation(LTI) partition of grid interface minimum traveltime
分 类 号:TP391.41[自动化与计算机技术—计算机应用技术] P315.31[自动化与计算机技术—计算机科学与技术]
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