Download programa cvm
Any idea what to remove? Like Like. You are commenting using your WordPress. You are commenting using your Google account. You are commenting using your Twitter account. You are commenting using your Facebook account.
Notify me of new comments via email. Aug 27, Aug 26, Aug 25, Aug 24, Aug 23, Aug 20, Aug 19, Aug 18, Aug 17, Aug 13, Aug 12, Aug 11, Aug 10, Aug 9, Aug 6, Aug 5, Aug 4, Aug 3, Aug 2, Jul 30, Jul 29, Jul 28, Jul 27, Jul 22, Jul 21, Jul 20, Jul 19, Jul 16, Jul 15, Jul 14, Jul 13, Jul 12, Jul 9, Jul 8, Jul 7, Jul 6, Jul 5, Jul 2, Jul 1, Jun 30, Jun 29, Jun 28, Jun 25, Jun 24, Jun 23, Jun 22, Jun 21, Jun 18, Jun 17, Jun 16, Jun 15, Jun 14, Jun 11, Jun 10, Jun 9, Jun 8, Jun 7, Jun 4, Jun 3, Jun 2, Jun 1, May 31, May 28, May 27, May 26, May 25, May 24, Release April 8, Date Added January 14, Version 1.
Operating Systems. Operating Systems iOS. Total Downloads 6. Downloads Last Week 0. Report Software. Related Apps. GarageBand Free. Turn your iPad, iPhone, and iPod touch into a full-featured recording studio. Netflix Free. The SCEC CVM-H velocity model describes seismic P- and S-wave velocities and densities, and is comprised of basin structures embedded in tomographic and teleseismic crust and upper mantle models.
This latest release of the CVM-H We recommend use of the most recent version of CVM-H, in most cases. Improvements in version This affects the boundary between the sediment and basement velocity parameterizations. Previous improvements that appeared in version The new Moho surface was compiled by Tape et al.
In replacing this surface care was taken that the depth interval around the Moho level both in the mantle and in the crustal portions of the model which were affected by this change, were assigned the correct domain, and consequently assigned velocities extrapolated from the underlying mantle model or from the crustal background model. In the offshore Santa Maria basin we extended the definition of the basement surface using reflection seismic data McIntosh et al.
We smoothly extrapolated sediment velocities from the onshore model into this new basinal area. Another basin, the relatively small San Bernardino basin, is now represented in the model.
0コメント