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Tables

 
Event Latitude Longitude Depth Event Latitude Longitude Depth
km km
9503141733 54.80 -161.40 33 9506291224 -19.46 169.24 144
9504072206 -15.20 -173.60 33 9506301158 24.62 -110.26 10
9504172328 45.90 151.30 33 9507031950 -29.20 -177.61 33
9504210517 12.20 126.30 33 9507081715 53.65 -163.55 33
9504230255 51.33 179.71 17 9507121546 -23.24 170.82 33
9504281630 44.07 148.00 29 9507262342 2.56 127.69 66
9505020606 -3.80 -76.90 120 9507270551 -12.58 79.24 10
9505050353 12.60 125.20 33 9508020014 -23.15 -70.58 33
9505130847 40.15 21.70 14 9508021105 -23.10 -70.41 33
9505162012 -22.90 169.70 33 9508030157 -23.13 -70.60 33
9505180006 -0.89 -22.00 12 9508030818 -28.35 -69.20 104
9505271303 52.63 142.83 11 9508041331 52.87 152.90 529
9506141111 12.20 -88.35 39 9508140437 -4.83 151.51 126
9506150015 38.40 22.27 14 9508161027 -5.81 154.21 16
9506211528 -61.62 154.71 10 9508161624 -5.42 153.76 21
9506240658 -3.98 153.94 386 9508162310 -5.78 154.26 74
9506250210 -3.28 150.37 45 9508192143 5.10 -75.69 125
9506271009 18.85 -81.73 10 9508230706 18.86 145.19 596
9506290745 48.78 154.46 62 9508281046 26.16 -110.35 10
Table 1 : Earthquakes Used in the Study


Locations determined by NEIC.


 
Station Name Latitude, tex2html_wrap_inline188 N Longitude, tex2html_wrap_inline188 W Operator
ADVT 44.32 72.49 Levin and Menke
BINY 42.19 75.99 USNSN
BLUE 43.89 74.45 ABBA
CLER 44.38 74.25 ABBA
GAC 45.70 75.48 CNSN
HRV 42.50 71.56 GSN
KEEN 44.26 73.82 ABBA
LBNH 44.24 71.93 USNSN
LSCT 41.68 73.22 USNSN
MDVB 43.99 73.18 Levin and Menke
MM01 42.32 72.71 MOMA
MM02 42.17 73.72 MOMA
MM03 42.04 74.85 MOMA
MM04 41.85 76.19 MOMA
NCB 43.97 74.22 LDEO
PACK 43.54 73.82 ABBA
PAL 41.00 73.91 IRIS and LDEO
STME 43.72 70.61 Levin and Menke
Table 2: Seismic Stations Used in the Study

In addition to permanent stations operated in the region by national and international networks we used some nodes of MOMA and ABBA portable broadband networks, and stations we deployed ourselves to compliment the coverage. See ( http://www.iris.washington.edu/PASSCAL/EasternUS.htm) for detailed descriptions.


 

depth (km) Vp, km/s Vs, km/s tex2html_wrap_inline234 ( tex2html_wrap_inline236 ) tex2html_wrap_inline238 () tex2html_wrap_inline240 () tex2html_wrap_inline242 () tex2html_wrap_inline244 () tex2html_wrap_inline246 () tex2html_wrap_inline248 ()
40 6.8 3.9 2.85 - - - - -
100 8.3 4.8 3.3 89 115 80 25 10 210
190 8.3 4.8 3.3 90 53 67 323 23 143
tex2html_wrap_inline250 8.3 4.8 3.3 - - - - -
Table 3: Anisotropic Structure (Orthorhombic Symmetry) Consistent With Shear Wave Splitting Observations at HRV

Velocity values in anisotropic layers are the isotropic averages of respective elastic tensors. The anisotropic medium is modeled as 30% orthorhombic olivine and 70% isotropic olivine, a mixture that is tex2html_wrap_inline180 6% anisotropic. The angles tex2html_wrap_inline230 and tex2html_wrap_inline182 define the tilt (from vertical) and azimuth (CW from N) of the symmetry axes (fast, intermediate, slow) within each anisotropic layer.


next up previous
Next: About this document Up: A Failed Search for Previous: Figure Captions

vadim levin
Tue Jun 8 20:49:14 EDT 1999