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宋根法,袁洪金,王卫华,高希勤,叶道凡:赛汉塔拉地区横波资料处理,《石油地球物理勘探》,23(4)1988:489～496近年来,地震勘探已从构造勘探阶段向岩性勘探方向迅速发展,地震工作已不满足于从纵波勘探资料中提取振幅、频率和其它信息,而希望从地震资料中直接得到岩性信息,研究地下的岩性各向异性、孔隙度和渗透率。借助于横波勘探,可以得到更多的反映地下岩性信息的资料,比如利用纵横波联合勘探可以得到速度比、泊松比和振幅比资料。应用这些资料可以进行碳氢检测、亮点检测,确定石灰岩的孔隙度。利用横波旅行
Song Genfa, Yuan Hongjin, Wang Weihua, Gao Xiqin, Ye Daofan: Transverse Wave Data Processing in Saihantala Area, Petroleum Geophysical Prospecting, 23 (4) 1988: 489-496 In recent years, seismic exploration has moved from the tectonic exploration stage to lithological exploration With rapid development and seismic work, it is no longer satisfactory to extract amplitude, frequency and other information from P-wave exploration data. Instead, it is hoped that lithological information will be obtained directly from seismic data to study the underground lithology anisotropy, porosity and permeability. With the help of S-wave exploration, more information can be obtained that can reflect the lithology information of the underground. For example, the data of velocity ratio, Poisson’s ratio and amplitude ratio can be obtained by using the combination of S-wave and S-wave exploration. Use these data for hydrocarbon detection, bright spot detection, and determination of limestone porosity. Traveling with S-waves