
Basic Geophysics - Processing IV: Migration
Author
Participating institute
Geophysikalisches Institut (GPI)
KIT-Zentrum Klima und Umwelt (ZKU)
Genre
Description
How are seismic signals from a particular period of time transformed in depth? Relationship between point-shaped scattering body and diffraction hyperbola, Kirchhoff migration principle.
Duration (hh:mm:ss)
00:10:44
Series
Brückenkurs Geophysik - Lernmodul Seismik / Basic Geophysics - Module Seismics
Published on
24.05.2019
Subject area
License
Creative Commons Attribution – NoDerivatives 4.0 International
Resolution | 1280 x 720 Pixel |
Aspect ratio | 16:9 |
Audio bitrate | 128000 bps |
Audio channels | 2 |
Audio Codec | aac |
Audio Sample Rate | 48000 Hz |
Total Bitrate | 933839 bps |
Color Space | yuv420p |
Container | mov,mp4,m4a,3gp,3g2,mj2 |
Media Type | video/mp4 |
Duration | 644 s |
Filename | DIVA-2019-450_hd.mp4 |
File Size | 75.188.103 byte |
Frame Rate | 25 |
Video Bitrate | 799744 bps |
Video Codec | h264 |
Media URL
Embed Code