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Thus, dense surveys between the existing profiles of MT stations are required for more detailed interpretations.
Seismologists predict that the dense surveys will yield precision imaging of magma chambers underneath volcanos and earthquake rupture zones along faults.
Taking advantage of cheap, long-lasting sensors developed by the oil and gas industry, seismologists are increasingly exploring the top 10 kilometers of the crust with dense surveys of hundreds or even thousands of seismometers.
Depth resolution of their surveys is unable to detect deeper fracture systems, but the precision of these lateral surveys to locate sharp boundaries indicates that dense surveys such as line H-1 with 5-m electrode spacing, and longer AB spreads, would be useful in further exploration.
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It later became clear that a more dense survey of variation in and around a gene was necessary to be confident that it has been adequately tested for association.
Since the analysis technique shown in this study does not require complex calculations and vast calculation times, it will be an effective technique for analyzing high-resolution data obtained densely by not only dense gravity surveys for fault research but also airborne gravity or gravity gradiometry surveys.
In addition, since this analysis technique does not require vast calculation times, I expect it will be an effective new technique for analyzing high-resolution data obtained densely, i.e., through dense gravity surveys for fault research and also airborne gravity gradiometry surveys.
Toyama City (2013) set three profiles crossing the Kurehayama Fault, and the dense gravity surveys of 50 m spaced measurements have been conducted on these profiles, although spacing of several hundred meters has been usually employed for these surveys.
A high reproducibility of the observed long-period ground motion at the middle and eastern parts of the Kanto Basin may be achieved by incorporating the S-wave velocity structures derived from dense microtremor surveys in Saitama, Ibaraki, and northern Chiba.
We converted the layered sedimentary structure models from dense microtremor surveys in Saitama, Ibaraki, and Chiba (Matsuoka and Shiraishi 2002; Yamanaka et al. 2005; Senna et al. 2013) using the same conversion procedure discussed above.
In dense gravity surveys researching fault structures in detail, profiles were set perpendicular to the fault and short-spaced gravity observations were taken along the profiles (e.g., Iwano et al. 2001; Inoue et al. 2004).
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