检索规则说明:AND代表“并且”;OR代表“或者”;NOT代表“不包含”;(注意必须大写,运算符两边需空一格)
检 索 范 例 :范例一: (K=图书馆学 OR K=情报学) AND A=范并思 范例二:J=计算机应用与软件 AND (U=C++ OR U=Basic) NOT M=Visual
作 者:Chen Meng Liu Jia-Hui Cui Yong-Fu Hu Tian-Yue Chen Fei-Xu Kuang Wei-Kang Zhang Zhen 陈猛;刘嘉辉;崔永福;胡天跃;陈飞旭;匡伟康;张振
机构地区:[1]Tarim Oilfi eld Company,PetroChina,Korla,Xinjiang 841000,China [2]School of Earth and Space Sciences,Peking University,Beijing 100871,China
出 处:《Applied Geophysics》2018年第3期491-499,共9页应用地球物理(英文版)
基 金:supported by the National Natural Science Foundation of China(No.41674122);National Science and Technology Major Project of China(No.2016ZX05004003);National Basic Research Program of China(No.2013CB228602)
摘 要:The attenuation of prestack internal multiples based on virtual seismic events is computationally costly and hinders seismic data processing. We propose a multiples attenuation method for poststack seismic data by approximating conventional virtual events. The proposed method is iterative. The proposed method is tested using 2D synthetic and the field poststack seismic datasets. Compared with the conventional virtual events method, the proposed method does not require data regularization and offers higher computation efficiency. The method requires to know the travel time of the primary reflection waves. The results of the application to 2D field datasets suggest that the proposed method attenuates the internal multiples while highlighting the deep primaries.基于虚同相轴原理的叠前层间多次反射波衰减技术的计算成本较高,在数据量较大时无法满足日增长的生产数据处理需求。针对该问题,提出了基于迭代算法的叠后虚同相轴预测层间多次波方法,并成功运用于二维叠后合成数据和实际地震数据。基于迭代算法的叠后虚同相轴方法需要一次反射波走时信息;相比于传统叠前虚同相轴方法,新方法增加了迭代计算过程,无需数据规则化,且具有更高的计算效率。实际陆上地震资料应用结果表明叠后虚同相轴方法能够显著衰减陆上层间多次波,突显深层一次波能量。
关 键 词:VIRTUAL EVENTS poststack INTERNAL multiple LAND SEISMIC data
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在载入数据...
正在链接到云南高校图书馆文献保障联盟下载...
云南高校图书馆联盟文献共享服务平台 版权所有©
您的IP:216.73.216.249