This is the publisher's version, also available electronically from "http://library.seg.org".Data from a shallow seismic‐source comparison test conducted in an area with a water‐table depth in excess of 30 m and near‐surface velocities less than 330 m/s were acquired from 13 different sources at a single site near Chino, California. The sources included sledgehammer, explosives, weight drop, projectile impacts, and various buffalo guns. A possible reflecting event can be interpreted at about 70 ms. At this particular test site, the lowly sledgehammer is among the best sources to provide data to see the possible reflection. Our previous work and that of our colleagues suggests that any source could dominate the comparison categories addresse...
calculate site response in the frequency band of 0.5–10 Hz at 24 locations in Los Gatos, California,...
The pyrotechnic materials are one of the types of the explosives materials which produce thermal, lu...
Abstract the density and seismic velocity of the medium, changes in either of which can cause a refl...
This is the publisher's version, also available electronically from "http://library.seg.org".A shall...
This is the publisher's version, also available electronically from "http://library.seg.org".We exam...
High-resolution shallow seismic reflection surveys require more attention to the choice of source an...
This is the publisher's version, also available electronically from "http://onlinelibrary.wiley.com"...
Different types of sources and receivers used with the seismic cone penetration test were investigat...
Pseudo walkaway noise tests were accomplished in study area in São Paulo city, Brazil, in order to e...
The shallow seismic reflection method plays an important role in helping to understand engineering, ...
The theoretical attractiveness of utilising both P- and S-reflection information is offset in the sh...
The pyrotechnic materials are one of the types of the explosives materials which produce thermal, lu...
Shallow seismic investigations were conducted at two sites in the Central Appalachian foreland area ...
In conjunction with crosswell seismic surveying being done at the Hanford Site in south-central Wash...
Ground motion generated by a magnitude 4.3 earthquake at Massachusetts Mountain on the Nevada Test S...
calculate site response in the frequency band of 0.5–10 Hz at 24 locations in Los Gatos, California,...
The pyrotechnic materials are one of the types of the explosives materials which produce thermal, lu...
Abstract the density and seismic velocity of the medium, changes in either of which can cause a refl...
This is the publisher's version, also available electronically from "http://library.seg.org".A shall...
This is the publisher's version, also available electronically from "http://library.seg.org".We exam...
High-resolution shallow seismic reflection surveys require more attention to the choice of source an...
This is the publisher's version, also available electronically from "http://onlinelibrary.wiley.com"...
Different types of sources and receivers used with the seismic cone penetration test were investigat...
Pseudo walkaway noise tests were accomplished in study area in São Paulo city, Brazil, in order to e...
The shallow seismic reflection method plays an important role in helping to understand engineering, ...
The theoretical attractiveness of utilising both P- and S-reflection information is offset in the sh...
The pyrotechnic materials are one of the types of the explosives materials which produce thermal, lu...
Shallow seismic investigations were conducted at two sites in the Central Appalachian foreland area ...
In conjunction with crosswell seismic surveying being done at the Hanford Site in south-central Wash...
Ground motion generated by a magnitude 4.3 earthquake at Massachusetts Mountain on the Nevada Test S...
calculate site response in the frequency band of 0.5–10 Hz at 24 locations in Los Gatos, California,...
The pyrotechnic materials are one of the types of the explosives materials which produce thermal, lu...
Abstract the density and seismic velocity of the medium, changes in either of which can cause a refl...