The Wonji Fault Belt is the active part of the Main Ethiopian Rift. In order to evaluate the deformation occurring along this part of the Rift a GPS network has been installed and measured during 3 campaigns covering a span of 3 years. The data have been processed using 2 different softwares. The results obtained are similar, the overall opening velocity of the WFB is 10 ± 4 mm/yr, although some of the inner benchmarks show even higher velocities.

Firuzabadì, D., Coltorti, M., Disperati, L., Salvini, R., Pizzi, A. (2009). GPS movements along the Wonji Fault Belt (Main Ethiopian Rift) [Misurazioni GPS lungo la Wonji Fault Belt (Main Ethiopian Rift)]. In Rendiconti online Soc. Geol. It., Atti del 3° Congresso Nazionale AIGA (pp.243-244). Roma : Società Geologica Italiana.

GPS movements along the Wonji Fault Belt (Main Ethiopian Rift) [Misurazioni GPS lungo la Wonji Fault Belt (Main Ethiopian Rift)]

Coltorti, M.;Disperati, L.;Salvini, R.;
2009-01-01

Abstract

The Wonji Fault Belt is the active part of the Main Ethiopian Rift. In order to evaluate the deformation occurring along this part of the Rift a GPS network has been installed and measured during 3 campaigns covering a span of 3 years. The data have been processed using 2 different softwares. The results obtained are similar, the overall opening velocity of the WFB is 10 ± 4 mm/yr, although some of the inner benchmarks show even higher velocities.
2009
Firuzabadì, D., Coltorti, M., Disperati, L., Salvini, R., Pizzi, A. (2009). GPS movements along the Wonji Fault Belt (Main Ethiopian Rift) [Misurazioni GPS lungo la Wonji Fault Belt (Main Ethiopian Rift)]. In Rendiconti online Soc. Geol. It., Atti del 3° Congresso Nazionale AIGA (pp.243-244). Roma : Società Geologica Italiana.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11365/18378