Coseismic and postseismic displacements from the 1978 Mw 7.3 Tabas-e-Golshan earthquake in eastern Iran
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文摘

Geodetic techniques for investigating earthquakes can be extended back to the 1970s.

We measured the co- and post-seismic displacements from the 1978 Tabas earthquake.

We show time-decaying shallow post-seismic afterslip following the 1978 earthquake.

The Tabas fold system may exhibit characteristic slip behaviour.

Such behaviour would require a magnitude Mw 7.3 earthquake every ∼3500 years.

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