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
机构地区:[1]大庆油田有限责任公司勘探开发研究院,黑龙江大庆163712
出 处:《大庆石油地质与开发》2012年第5期158-162,共5页Petroleum Geology & Oilfield Development in Daqing
基 金:国家重点基础研究发展计划“973”项目(2009CB219307).
摘 要:为了消除地震资料中不同炮检距、不同入射角信息对地震振幅特征的影响,从地震反射系数与地质界面的波阻抗关系出发,根据研究区地层构造相对平缓的特点建立了针对平缓地层的窄入射角成像方法,通过入射角计算、入射角带生成和共入射角成像得到了储层非均质特征明显的高精度地震数据体。与原处理成果对比结果表明,窄入射角成像结果岩性边界清晰,沿层地震属性河道砂体展布特征明显,与地质研究成果更加吻合。该方法对于储层构造形态相对平缓的地区具有较好的应用前景。In order to eliminate the influences of different geophone offsets and different incident angles on the seis- mic amplitude characteristics in seismic data, from the viewpoint of the wave impedance relations between the seis- mic reflection coefficients and geological interfaces, according to the characteristics of relatively flat stratigraphic structures in study area, the method of the narrow incident angle imaging is established in the light of the flat lay- ers. Through the incident angle calculation, incident-angle band generation and common incident-angle imaging, the high-precision seismic data bodies are got with obvious heterogeneity characteristics of the reservoirs. Compared with the original processed results, the fact show that the narrow incident-angle imaging is characterized by the clear lithology boundary and distinct spread property of channel sandbody along the seismic attributes of the formations, and furthermore the achievements stated above are identical with the results of the geological study. This method possesses much better application prospects for the region with relatively flat reservoir structural configuration.
分 类 号:P631[天文地球—地质矿产勘探]
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:216.73.216.4