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Figure S1. Complete data records for (A) event 20101103, (B) event 20081217, and (C) event 20110519. The selected representative records for the whole array are displayed in Fig. 1. Figure S2. Comparison between the P data and synthetics for the model proposed by Savage (2012). Figure S3. Sensitive test for models with different slab heterogeneities characterized by different a x ,a z , and σ p in von Kármán distribution function. The numbers on top of synthetics frames are width of the slab, a x ,a z , and σ p . Figure S4. Test for the attenuation effects. Comparing to the model without considering attenuation (A), an attenuated model (B) shows significant amplitude drop, especially at the smaller distance while rays sample the low-Q mantle wedge. (C) shows the same seismograms in (B) but with amplitude amplified by 2. Note the waveforms in (C) are almost identical as those in (A) at distance larger than 0.6°. The red dash line in (A) displays the LVL trapped high frequency arrivals, which is not shown for the attenuated model. Figure S5. Comparison between the synthetics without and with attenuation. The attenuation is added by applying t* correction assuming Q = 700. Figure S6 Spectrograms for the data and synthetics for models with different slab heterogeneities characterized by different a x ,a z , and σ p . Figure S7. Sensitive test for models with different extended depth of the LVL. Figure S8. Sensitive test for models with different width of the slab. Figure S9. Sensitive test for models with different slab dipping angle.

Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

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Page 1: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

Figure S1. Complete data records for (A) event 20101103, (B) event 20081217, and (C)

event 20110519. The selected representative records for the whole array are displayed in

Fig. 1.

Figure S2. Comparison between the P data and synthetics for the model proposed by

Savage (2012).

Figure S3. Sensitive test for models with different slab heterogeneities characterized by

different ax, az, and σp in von Kármán distribution function. The numbers on top of

synthetics frames are width of the slab, ax, az, and σp.

Figure S4. Test for the attenuation effects. Comparing to the model without considering

attenuation (A), an attenuated model (B) shows significant amplitude drop, especially at

the smaller distance while rays sample the low-Q mantle wedge. (C) shows the same

seismograms in (B) but with amplitude amplified by 2. Note the waveforms in (C) are

almost identical as those in (A) at distance larger than 0.6°. The red dash line in (A)

displays the LVL trapped high frequency arrivals, which is not shown for the attenuated

model.

Figure S5. Comparison between the synthetics without and with attenuation. The

attenuation is added by applying t* correction assuming Q = 700.

Figure S6 Spectrograms for the data and synthetics for models with different slab

heterogeneities characterized by different ax, az, and σp.

Figure S7. Sensitive test for models with different extended depth of the LVL.

Figure S8. Sensitive test for models with different width of the slab.

Figure S9. Sensitive test for models with different slab dipping angle.

Page 2: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

20101103

15 sec

Figure S1

(A)

Page 3: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

Figure S1

(B)

20081217

15 sec

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Figure S1

(C)

20110519

15 sec

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Data

Figure S2

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(A) Velocity envelope

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Data 80km/10/0.5/2.5 80km/10/1/2.5 80km/5/1/2.5

Figure S3

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(A) Velocity envelope

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Data 80km/5/0.5/2.5 80km/20/1/2.5 80km/2.5/2.5/2.5

Figure S3continued

Page 8: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

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Without attenuation With attenuation With attenuationAmplitude × 2

(A) (B) (C)

Figure S4

Page 9: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

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(A) Velocity envelope

(B) Velocity

Data 80km/10/0.5/2.5no Q

80km/10/0.5/2.5Q = 700

Figure S5

Page 10: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

0

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Hz)

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36 38 40 42 44 46 48 50 52 54

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80km/20/1/2.5 80km/2.5/2.5/2.5

0.0 0.2 0.4 0.6 0.8

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Figure S6

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(A) Velocity envelope

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Data 80km/10/0.5/2.5LVL to 100km

80km/10/0.5/2.5LVL to 300 km

Figure S7

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Data 80km/10/0.5/2.5 50km/10/0.5/2 110km/10/0.5/3

Figure S8

Page 13: Figure S1. - CaltechAUTHORSauthors.library.caltech.edu/45612/7/mmc1.pdf · 2014. 5. 8. · Figure S1.Complete data records for (A) event 20101103, (B) event 20081217, and (C) event

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(A) Velocity envelope

(B) Velocity

Data 80km/10/0.5/2.5Dip angle = 75°

50km/10/0.5/2.5Dip angle = 70°

110km/10/0.5/2.5Dip angle = 80°

Figure S9