Shallow geological structures triggered during the Mw 6.4 Meinong earthquake, southwestern Taiwan
The Meinong earthquake generated up to ~10 cm surface displacement located 10 - 35 km west of the epicenter and monitored by InSAR and GPS. In addition to coseismic deformation related to the deep earthquake source, InSAR revealed three sharp surface displacement gradients. One of them is extensiona...
Збережено в:
| Автори: | , , , , , , , , , , |
|---|---|
| Формат: | Artigo |
| Мова: | Inglês |
| Опубліковано: |
Springer
2017-01-01
|
| Серія: | Terrestrial, Atmospheric and Oceanic Sciences |
| Онлайн доступ: |
http://tao.cgu.org.tw/media/k2/attachments/v285p663.pdf
|
| Теги: |
Немає тегів, Будьте першим, хто поставить тег для цього запису!
|