Geophysical ProspectingVolume 58, Issue 3 p. 539-539 Free Access Errata This article corrects the following: On the accuracy of the ground force estimated in vibroseis acquisition Christos Saragiotis, Péter Scholtz, Claudio Bagaini, Volume 58Issue 1Geophysical Prospecting pages: 69-80 First Published online: December 11, 2009 Source measurement effect on high fidelity vibratory seismic separation Nirupama Nagarajappa, David Wilkinson, Volume 58Issue 1Geophysical Prospecting pages: 55-68 First Published online: October 30, 2009 How do hydraulic vibrators work? A look inside the black box John J. Sallas, Volume 58Issue 1Geophysical Prospecting pages: 3-18 First Published online: October 30, 2009 Reflection point sideslip and smear in imaging below dipping anisotropic media Rob Vestrum, Don Lawton, Volume 58Issue 4Geophysical Prospecting pages: 541-548 First Published online: December 1, 2009 First published: 26 March 2010 https://doi.org/10.1111/j.1365-2478.2010.00878.xAboutSectionsPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onFacebookTwitterLinked InRedditWechat In [[1] ] equation (3) currently reads: (3) It should read: (3) The only error has to do with the term F that should have appeared as lower case f to represent the instantaneous frequency in Hz, as defined in the sentence above this equation. In [[2] ] some symbols are missing. On page 56, equation (1) currently reads: (1) It should read: (1) The following sentence published on page 58: For example, if the response of vibrator 2 during sweep 2 is delayed by seconds with respect to sweep 1 response, then the value of k for element [2, 2] of the matrix A (Fig. 3b) would be e−i2πf. Should read: For example, if the response of vibrator 2 during sweep 2 is delayed by τ seconds with respect to sweep 1 response, then the value of k for element [2, 2] of the matrix A (Fig. 3b) would be e−i2πfτ. In [[3] ] equation (3) reads: (3) It should read: (3) q has been defined earlier in the text as a quantity that models the frequency-dependent effects (other than the Earth itself) due to the receivers, recording equipment, attenuation etc., while here the quantity models the actual groundforce and should therefore be g. In [[4] ] the incorrect caption for Fig. 8 was published. The correct caption for this figure should read: Figure 8 Isotropically migrated stacks of limited-offset ranges from the 15° model data: a) near offsets from 0–1300 m, b) mid offsets from 1300–2600 m, c) far offsets from 2600–4500 m. The horizontal line represents the model position of the reflector. The vertical markers indicate an estimate of the horizontal position of the reflector edge on each of the three limited-offset images: near, mid and far. REFERENCES [1] Sallas J.J. 2010. How do hydraulic vibrators work? A look inside the black box. Geophysical Prospecting 58, 3– 17. doi:10.1111/j.1365-2478.2009.00837.xWiley Online LibraryWeb of Science®Google Scholar [2] Nagarajappa N. and Wilkinson D. 2010. Source measurement effect on high fidelity vibratory seismic separation. Geophysical Prospecting 58, 55– 67. doi:10.1111/j.1365-2478.2009.00839.xWiley Online LibraryWeb of Science®Google Scholar [3] Saragiotis C., Scholtz P. and Bagaini C. 2010. On the accuracy of the ground force estimated in vibroseis acquisition. Geophysical Prospecting 58, 69– 80. doi:10.1111/j.1365-2478.2009.00851.xWiley Online LibraryWeb of Science®Google Scholar [4] Vestrum R. and Lawton D. 2009. Reflection point sideslip and smear in imaging below dipping anisotropic media. Geophysical Prospecting. doi:10.1111/j.1365-2478.2009.00849.xWiley Online LibraryWeb of Science®Google Scholar Volume58, Issue3May 2010Pages 539-539 ReferencesRelatedInformation