Holocene rockfalls in the southern Negev Desert, Israel and their relation to Dead Sea fault earthquakes
Rockfall ages in tectonically active regions provide information regarding frequency and magnitude of earthquakes. In the hyper-arid environment of the Dead Sea fault (DSF), southern Israel, rockfalls are most probably triggered by earthquakes. We dated rockfalls along the western margin of the DSF...
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Veröffentlicht in: | Quaternary research 2014-03, Vol.81 (2), p.260-273 |
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