Station XF L25 - XF.L25

Network: XF00 - Laramie Telemetered Brad-band Array

Nearby stations (2 deg radius)

Station Name (Lat, Lon) Start / End Elevation
L25 XF.L25 (41.48, -105.93) 2000-09-01 / 2002-01-01 1.8 m
Crust2 Type:P4,orogen/50km, Urals, Tethian Orogen, Rockies 1 km seds.
Thickness Estimate:65 km
Thickness StdDev:11 km
Vp/Vs Estimate:1.67
Vp/Vs StdDev:0.15
Vs Estimate:3.782 km/s
Poisson's Ratio:0.22
Peak Value:0.10
Assumed Vp:6.306 km/s
Ps Weight:0.33333334
PpPs Weight:0.33333334
PsPs Weight:0.33333328
Residual Complexity:0.687
Nearby stations H: +-
(2.0 deg) Vp/Vs: +-

0 with match > 90% ( 0.0 %) and 3 with match > 80% ( 100.0 %) out of 3.

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Azimuth Distribution of Events:

Prior Results for this Station

Study Thickness Vp/Vs Vp Vs Poissons Ratio Extra
EARS 65 km 1.67 6.306 km/s 3.782 km/s 0.22
Crust2.0 50 km 1.76 6.306 km/s 3.584 km/s 0.26 P4,orogen/50km, Urals, Tethian Orogen, Rockies 1 km seds.
Global Maxima 65 km 1.67 6.306 km/s 3.782 km/s 0.22 amp=0.102367535
Local Maxima 1 46 km 1.90 6.306 km/s 3.31 km/s 0.31 amp=0.074123554
Local Maxima 2 68 km 1.61 6.306 km/s 3.911 km/s 0.19 amp=0.036632344
Local Maxima 3 48 km 1.81 6.306 km/s 3.489 km/s 0.28 amp=0.024701517
Local Maxima 4 66 km 2.10 6.306 km/s 3.006 km/s 0.35 amp=0.020031469
Predicted Arrivals for vertical incidence
(zero ray parameter)
Ps6.88 SECOND
PpPs27.50 SECOND
PsPs/PpSs34.38 SECOND

Events Processed for this Station

Download zip of receiver functions as SAC

View Record Section

Plot maxima for each earthquake.

Events Used in the Stack

(3 events)
Radial Match Distance Baz FERegion Time Lat/Lon Depth Magnitude
86.97247 32.1 deg 147.002 deg El Salvador 2001/01/13 17:33:32 GMT (13.0, -88.7) 60 km 6.4 MB, 7.8 MS, 7.7 MW, 7.5 ME
80.1661 97.4 deg 14.911 deg Turkmenistan 2000/12/06 17:11:06 GMT (39.6, 54.8) 30 km 6.7 MB, 7.5 MS, 7.0 MW, 6.9 ME
80.05511 47.4 deg 144.454 deg Near Coast Of Ecuador 2000/09/28 23:23:43 GMT (-0.2, -80.6) 23 km 5.8 MB, 6.0 MS, 6.6 MW, 6.4 MW

Losers

(0 events)
Radial Match Distance Baz FERegion Time Lat/Lon Depth Magnitude Reason