Active faulting within a megacity: the geometry and slip rate of the Pardisan thrust in central Tehran, Iran
Tehran, the capital city of Iran with a population of over 12 million, is one of the largest urban centres within the seismically active Alpine-Himalayan orogenic belt. Although several historic earthquakes have affected Tehran, their relation to individual faults is ambiguous for most. This ambigui...
| Asıl Yazarlar: | , , , , , , , |
|---|---|
| Materyal Türü: | Journal article |
| Baskı/Yayın Bilgisi: |
Oxford University Press
2016
|