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Euler, G.G., Wiens, D.A., Shore, P., Koch, F.W., Tibi, R., Nyblade, A.A. and Reusch, A.M. (2008) Shear Velocity Structure of the Cameroon Volcanic Line Region from Rayleigh Wave Phase Velocities. EOS, Transactions, American Geophysical Union, AGU Fall Meeting Suppl., 89, Abstract #S21C-1843.

has been cited by the following article:

• TITLE: Fault-Plane Solution of the Earthquake of 19 March 2005 in Monatele (Cameroon)

  AUTHORS: Eric N. Ndikum, Charles T. Tabod, Alain-Pierre K. Tokam, Bernard Z. Essimbi

  KEYWORDS: Earthquake, Monatele, Epicenter, Fault Plane Solution, Strike-Slip Fault, Normal Faulting, Component

  JOURNAL NAME: Open Journal of Geology, Vol.4 No.6, June 23, 2014

  ABSTRACT: An earthquake of magnitude Ml = 3.04 was detected on the 19 of March 2005 at 11:49:18.31 (local time) by seven broadband seismometers located around Cameroon (Central Africa). Its epicenter has been relocated and found to be in Monatele (Cameroon) with latitude 4°26.34' and longitude 10°59.62'. The fault-plane solution calculated using double couple fault-plane solutions based on P-wave polarity readings, also taking into consideration the dextral nature of the Sanaga Fault (SF) underlying this region of the epicenter, is a strike-slip fault with a normal faulting component. The beach ball representation of this fault-plane solution has strike, dip and rake values of 289, 70, -169 for the principal fault plane and 195, 80, -20 for the auxiliary fault plane.