成都理工大学学报(自然科学版)
成都理工大學學報(自然科學版)
성도리공대학학보(자연과학판)
JOURNAL OF CHENGDU UNIVERSITY OF TECHNOLOGY(SCIENCE & TECHNOLOGY EDITION)
2009年
4期
434-442
,共9页
三维地质建模%地质块体%三角网%射线追踪%高斯射线束正演
三維地質建模%地質塊體%三角網%射線追蹤%高斯射線束正縯
삼유지질건모%지질괴체%삼각망%사선추종%고사사선속정연
3-D geologic modeling%geologic block%triangle net%ray tracing%Gaussian beam forward
提出了一种利用二维地质剖面构建三维块状地质模型的方法.该方法以用户编辑的二维地质剖面为输入,寻找地质块体的拓扑关系,自动构建以地质块体为单元的块状三维地质模型.在三维块状模型的基础上,研究了三维高斯射线束正演方法.这是一种快速的地震记录合成方法,它将波动方程和射线理论紧密结合起来,通过运动学射线追踪获取射线轨迹,通过动力学追踪来获取中心射线附近的高频能量分布,因而既能反映波的运动学特征,又能表现波的动力学特点,并且具有运算速度快、精度高等优点.
提齣瞭一種利用二維地質剖麵構建三維塊狀地質模型的方法.該方法以用戶編輯的二維地質剖麵為輸入,尋找地質塊體的拓撲關繫,自動構建以地質塊體為單元的塊狀三維地質模型.在三維塊狀模型的基礎上,研究瞭三維高斯射線束正縯方法.這是一種快速的地震記錄閤成方法,它將波動方程和射線理論緊密結閤起來,通過運動學射線追蹤穫取射線軌跡,通過動力學追蹤來穫取中心射線附近的高頻能量分佈,因而既能反映波的運動學特徵,又能錶現波的動力學特點,併且具有運算速度快、精度高等優點.
제출료일충이용이유지질부면구건삼유괴상지질모형적방법.해방법이용호편집적이유지질부면위수입,심조지질괴체적탁복관계,자동구건이지질괴체위단원적괴상삼유지질모형.재삼유괴상모형적기출상,연구료삼유고사사선속정연방법.저시일충쾌속적지진기록합성방법,타장파동방정화사선이론긴밀결합기래,통과운동학사선추종획취사선궤적,통과동역학추종래획취중심사선부근적고빈능량분포,인이기능반영파적운동학특정,우능표현파적동역학특점,병차구유운산속도쾌、정도고등우점.
The ray method plays a vital role in seismic exploration. The 3-D block geological model is the base of the ray numerical modeling. However the 3-D geological modeling, especially the complex model structure usually is quite difficult. This paper proposes an algorithm to use two-dimensional geological cross section to construct the three dimensional geological model. The algorithm has effectively solved the complex geological modeling problem. Based on the first hand information about 2-D geological cross section edited by users, the method researches the topology of geological blocks and automatically structures model on 3-D geological blocks. With the 3-D block geological model, the authors deeply research the numerical modeling method of Gaussian Beam. Gaussian beam method is a fast method of seismic wave field modeling. The seismic wave field obtained by this method has wave properties in both kinematics and high-frequency dynamic. By merging wave equation with the ray theory, the method obtains ray tracks by the kinematical ray tracing and distribution of high-frequency by the dynamic ray tracing. As a result, it has the dynamic and geometric characters and costs little calculation time, and shows good precision.