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PDF file - Laboratoire de Géologie de l'Ecole normale supérieure - Ens

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VIGNY ET AL.: ARABIA PLATE MOTION<br />

Figure 2. Large scale velocities in the ITRF2000 reference frame, relative to Eurasia as <strong>de</strong>fined by Calais et al.<br />

(2003). Ellipses show the 99% confi<strong>de</strong>nce level of the a-priori formal uncertainties given in table 2. Numbers next<br />

to arrow heads indicate the station velocity in mm/yr.<br />

Somalia<br />

The motion of Somalia is constrained by even less<br />

data than Africa: only two sites (MALI and SEY1)<br />

were used by Sella et al. [2002], making the<br />

7<br />

<strong>de</strong>termination of the pole unambiguous, but not well<br />

constrained. Fernan<strong>de</strong>s et al. [2003] used four sites<br />

(MALI, SEY1, REUN and RBAY). We did not use<br />

RBAY in our computations because no data was<br />

available during the various campaigns, but we ad<strong>de</strong>d<br />

three sites of the Djibouti regional network which are

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