Two regions of seafloor deformation generated the tsunami for the 13 November 2016, Kaikoura, New Zealand earthquake
Abstract The 13 November 2016 Kaikoura, New Zealand, Mw 7.8 earthquake ruptured multiple crustal faults in the transpressional Marlborough and North Canterbury tectonic domains of northeastern South Island. The Hikurangi trench and underthrust Pacific slab terminate in the region south of Kaikoura,...
שמור ב:
| Principais autores: | , , , |
|---|---|
| פורמט: | Artigo |
| שפה: | Inglês |
| יצא לאור: |
Wiley
2017-07-01
|
| סדרה: | Geophysical Research Letters |
| נושאים: | |
| גישה מקוונת: | https://doi.org/10.1002/2017GL073717 |
| תגים: |
אין תגיות, היה/י הראשונ/ה לתייג את הרשומה!
|