aGeodetic reference plate for MORVEL. Plate abbreviations are defined in fig. 1 of DeMets et al. (2010). Angular velocities describe counter-clockwise rotation of the given plate relative to either ITRF2000 or ITRF2005. All site velocities were adjusted for geocentral translation prior to the estimate of the best-fitting angular velocities, as described in the text. Cartesian covariances are propagated from the GPS velocity uncertainties and have units of 10−8 rad2 Myr−2. Additional information about the covariances is given in the footnotes to table 1 of DeMets et al. (2010).
Version of Record online: 24 AUG 2011
© 2011 The Authors Geophysical Journal International © 2011 RAS
Geophysical Journal International
Volume 187, Issue 1, page 538, October 2011
How to Cite
(2011), Erratum. Geophysical Journal International, 187: 538. doi: 10.1111/j.1365-246X.2011.05186.x
- Issue online: 19 SEP 2011
- Version of Record online: 24 AUG 2011
Vol. 181, Issue 1, 1–80, Version of Record online: 24 FEB 2010
DeMets, C., Gordon, R.G., & Argus, D.F., 2010. Geologically current plate motions (Geophys. J. Int., 181, 1–80, doi: 10.1111/j.1365-246X.2009.04491.x).
This erratum corrects several typographical and/or transcription errors in DeMets et al. (2010), as follows. (1) The GPS-derived angular velocities and covariances in Table 4 on p. 58 of DeMets et al. (2010) were transcribed incorrectly into the original manuscript from their computer source files. Table 4 is amended herein and fully replaces the original Table 4. None of the transcription errors in Table 4 affect the MORVEL angular velocity estimates or any of the other calculations in the original paper. (2) All velocities given in paragraph 2 of section 5.8.2 (p. 61) for the movement of the Caribbean plate relative to the South America plate along the Central Range fault of Trinidad (10.4°N, 61.2°W) instead specify motion of the South America plate relative to a fixed Caribbean plate. In the same paragraph, the 20.0 ± 0.5 mm yr−1 (1σ), S78.2°W±1.3° velocity that is predicted at 10.4°N, 61.2°W by the MORVEL South America–Caribbean plate angular velocity was inadvertently determined using an out-of-date angular velocity estimate and should instead be 20.4 ± 0.4 mm yr−1 (1σ) toward S76.5°W±1.4°. The new velocity resolves into fault-parallel and fault-normal components of 20.2 ± 0.4 mm yr−1 and 3.0 ± 0.5 mm yr−1 along the N68°E-striking Central Range fault, slightly different than the values of 19.6 ± 0.5 mm yr−1 and 3.5 ± 0.5 mm yr−1 that are cited near the end of the same paragraph. (3) The first sentence in section 5.6.6 incorrectly states that there are 68 seafloor spreading rates from the Pacific-Cocos plate boundary. There are instead 61 spreading rates. (4) Finally, the exclamation point within the text string ‘NA!SA’ in fig. 25 should instead be a hyphen.
|Plate||Num.||Angular velocity||Variances and covariances|
|stations||Lat. (°N)||Long. (°E)||ω (deg Myr−1)||σxx||σxy||σxz||σyy||σyz||σzz|
- 2010. Geologically current plate motions, Geophys. J. Int., 181, 1–80, doi: 10.1111/j.1365-246X.2009.04491.x. , & ,
Supplement. Text versions of tables 1, 2, 3, 5 and 6 from DeMets et al. (2010) and a text version of the amended Table 4 displayed in this erratum.
|GJI_5186_sm_SuppMat.txt||23K||Supporting info item|
Please note: Wiley Blackwell is not responsible for the content or functionality of any supporting information supplied by the authors. Any queries (other than missing content) should be directed to the corresponding author for the article.