共接收面元三维折射旅行时反演方法
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  • 英文篇名:3D refraction traveltime inversion in common-receiver-bins
  • 作者:金昌昆 ; 张建中
  • 英文作者:Jin Changkun;Zhang Jianzhong;Key Laboratory of Submarine Geosciences and Prospecting Techniques, Ministry of Education;College of Marine Geosciences,Ocean University of China;Laboratory for Marine Mineral Resources,Qingdao National Laboratory for Marine Science and Technology;
  • 关键词:折射旅行时 ; 共接收面元 ; 共方位角道集 ; 静校正
  • 英文关键词:refraction traveltime;;common-receiver bin;;common-azimuth gather;;statics
  • 中文刊名:SYDQ
  • 英文刊名:Oil Geophysical Prospecting
  • 机构:海底科学与探测技术教育部重点实验室;中国海洋大学海洋地球科学学院;海洋国家实验室海洋矿产资源评价与探测技术功能实验室;
  • 出版日期:2016-08-15
  • 出版单位:石油地球物理勘探
  • 年:2016
  • 期:v.51
  • 基金:国家自然科学基金项目(41074077、41230318);; 高等学校博士学科点专项科研基金资助课题(20130132110023)联合资助
  • 语种:中文;
  • 页:SYDQ201604017
  • 页数:11
  • CN:04
  • ISSN:13-1095/TE
  • 分类号:8-9+124-132
摘要
本文提出一种基于共接收面元的三维折射旅行时反演方法。将工区划分成若干个接收面元,并设每个接收面元内高速层速度不变。先根据折射时距曲线瞬时斜率计算各个接收面元的高速层速度。对于一个接收面元,把各炮点与该接收面元有关的炮检距和折射旅行时数据按方位角划分成共方位角道集,分别将各共方位角道集数据转换成相对于均值的相对坐标数据,再对该接收面元的所有相对坐标数据进行直线拟合,将拟合直线斜率的倒数作为该接收面元内的高速层速度。求出各个接收面元的折射速度后,根据折射旅行时方程得到各对炮点和接收点的延迟时间之和,构成所有炮点和接收点延迟时间满足的线性方程组,在平滑约束下用最小平方QR分解(LSQR)算法解该方程,获得各炮点和接收点的延迟时间。用该方法对新疆A区山前带的三维地震资料进行长波长静校正处理,取得了良好的应用效果。
        In this paper,an approach to 3D refraction traveltime inversion is proposed.First,work area is divided into common-receiver-bins(CRBs),and velocity of high-velocity layer for all bins is assumed to be constant.Velocity of the high-velocity layer for every CRB is calculated on instantaneous slopes of refraction time-distance curves.Then common azimuth gathers(CAG)are extracted from refraction data for a CRB based on traveltimes and offsets,and they are transformed into coordinate data based on their arithmetic mean values.After that,coordinate data in a CRB are fitted by least-square straight line and instantaneous slope of refraction time-distance curves is obtained.The reciprocal of this instantaneous slope is taken as velocity of high-velocity layer.After velocity for all CRBs is estimated,delay times for all source-receiver pairs can be calculated from refraction traveltime equations,which form a large linear equation.Finally delay times for each source and receiver are estimated by solving the equation set with smoothness constraint LSQR algorithm.Field data applications show that the proposed approach calculates accurately long-wavelength static corrections for 3D seismic data from a foothill belt in Xinjiang,West China.
引文
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