GPS estimates of microplate motions, northern Caribbean: evidence for a Hispaniola microplate and implications for earthquake hazard
Version of Record online: 25 SEP 2012
© 2012 The Authors Geophysical Journal International © 2012 RAS
Geophysical Journal International
Volume 191, Issue 2, pages 481–490, November 2012
How to Cite
Benford, B., DeMets, C. and Calais, E. (2012), GPS estimates of microplate motions, northern Caribbean: evidence for a Hispaniola microplate and implications for earthquake hazard. Geophysical Journal International, 191: 481–490. doi: 10.1111/j.1365-246X.2012.05662.x
- Issue online: 9 OCT 2012
- Version of Record online: 25 SEP 2012
- Accepted 2012 August 31. Received 2012 August 27; in original form 2012 April 16
Figure S1. Elastic (a) and rotational (b--d) components of GPS velocities based on best-fitting model. Scale is in upper right corner of all panels. (a) Best-fitting elastic component of GPS velocities estimated with blocks. These velocities show the elastic effects of fault locking, independent of the rotational component (b--d). (b) GPS velocities relative to Gônave microplate corrected for elastic effects shown in (a). Velocities thus illustrate rotational component of the site motions, independent of the elastic effects associated with locked faults. Scale is in upper right corner. (c) Same as B but fixed North America plate. (d) Same as (b) but fixed Hispaniola plate.
Table S1. GPS velocities with respect to the Caribbean plate.
|GJI_5662_sm_Supplement.zip||928K||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.