2 edition of three-component seismic refraction survewy in Northwestern Arizona found in the catalog.
three-component seismic refraction survewy in Northwestern Arizona
Vivian K. Hussey
Written in English
|Statement||by Vivian K. Hussey.|
|Contributions||Boston College. Dept. of Geology and Geophysics.|
|The Physical Object|
|Pagination||iii, 161 leaves :|
|Number of Pages||161|
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The seismic survey was performed using an IVI "Minivib 1" source with a "landstreamer" three-component geophone array built by the GSC. The landstreamer consists of. FIG. Generalized geological map of northwestern South Three-component seismic refraction survewy in Northwestern Arizona book.
The region of study, the Western Cordillera, (~), extends from southern Ecuador to 8°N in Colombia. Seismic refraction profiles: Yumbo Quarry-North (, this paper), Yumbo Quarry-West [ (Meissner et al, ; and ,File Size: 1MB.
The 2-D three-component seismic lines were acquired by Enertec Geophysical Services Ltd. with support from Geo-X Systems Ltd. (Figure 4). The survey was somewhat complicated but the contractors performed very ably.
The ARAM recording system was chosen as it could record to less than I Hz, had a high channel capability, and used bit sampling. The number of broadband three-component seismic stations in southern California has more than tripled recently.
In this study we use the teleseismic receiver function technique to determine the crustal thicknesses and V_p/V_s ratios for these stations and map out the lateral variation of Moho depth under southern California. It is shown that a receiver function can provide a very Cited by:  Refraction traveltimes from a 46‐km long seismic survey across the San Andreas Fault were inverted to obtain two‐dimensional velocity structure of the upper crust near the SAFOD drilling project.
The model contains strong vertical and lateral velocity variations from Cited by: VTI anisotropy has been proven to have a large impact on the location accuracy of microseismic events associated with hydraulic fracture monitoring (e.g., Erwemi et al.,Maxwell et al., ).
However, the influence of HTI anisotropy on. The deployment of a dense seismic array of portable broadband stations has presented a number of imaging opportunities using scattered teleseismic waves.