作者: R. R. Stewart
DOI: 10.1190/1.1442445
关键词:
摘要: Laboratory measurements and field experiments indicate that many sedimentary rocks display velocity anisotropy (Robertson Corrigan, 1983; White et al., Thomsen, 1986; Winterstein, Gaiser 1987). Accounting for is proving important in several areas including the processing interpretation of shear‐wave data (Lynn Bush Crampin, 1987) integration vertical seismic profile (VSP) surface (Chiu Stewart, 1987a).