Table 2 Crustal anisotropy from joint analysis of R and T- components of receiver function and SKS splitting results for the five teleseismic stations in Somaliland.
From: Crustal structure and seismic anisotropy of rift basins in Somaliland
Station | Crustal anisotropy | SKS splitting | ||||
|---|---|---|---|---|---|---|
Crust | Upper layer | Lower layer | ||||
ϕ (°) | \(\delta t\)(s) | ϕ (°) | \(\delta t\)(s) | ϕ (°) | \(\delta t\)(s) | |
Eil Daraad | 80 ± 8 | 0.4 ± 0.10 | 80 | 0.4 | 50 | 1.3 |
Hagal | 75 ± 10 | 0.4 ± 0.20 | 70 | 0.4 | 55 | 1.1 |
Burao | − 15 ± 6 | 0.4 ± 0.05 | − 28 | 0.4 | 50 | 1.0 |
Haydh | − 85 ± 8 | 0.3 ± 0.20 | − 85 | 0.4 | 54 | 1.1 |
Dharyeley | − 85 ± 10 | 0.4 ± 0.10 | − 85 | 0.4 | 56 | 0.7 |
