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Volumn 277, Issue 5326, 1997, Pages 667-670

Observations of PKKP precursors used to estimate small-scale topography on the core-mantle boundary

Author keywords

[No Author keywords available]

Indexed keywords

CORE/MANTLE BOUNDARY; PKKP PHASE; TOPOGRAPHY;

EID: 0030881835     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.277.5326.667     Document Type: Article
Times cited : (63)

References (47)
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    • Including seismograms with impulsive noise bursts resulting from unrelated earthquakes or instrument error would contaminate the stacked image. Seismograms containing such artifacts were removed by visual inspection. In addition, possible contamination from double events was further avoided by removing traces with impulsive energy arriving before the theoretical P arrival. Other seismic phases, including SS, SP, and SPP, overlap a portion of the time-distance window in which the precursors were imaged. However, these phases have a different move-out and are not consistently observed at high frequencies (11) because of the high attenuation of the S phase.
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    • Eighty-nine percent of the CMB is within 10° of a PKKP underside CMB reflection point. However, 83% of the reflection points are in the Southern Hemisphere, due to a concentration of seismic stations in the Northern Hemisphere.
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    • We subtracted the average noise from a 60-s window starting 140 s before the PKKPbc arrival. Shifting the noise window to a time that overlaps with the precursory wave train changes the precursors' zero offset but not their shape.
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    • The weight assigned to a processed trace was defined as the ratio of the maximum value found in a signal window to that taken in a noise window. An incorrect choice for the position of the noise window can bias the amplitude of the precursors, highlighting the importance of the P-wave test (Fig. 2C). A gap between the end of the noise window and the start of the reference phase will falsely amplify the observed precursors by ∼5%. This was verified in stacks using P as a reference phase. A false precursory wave train was imaged, for distance ranges with poor STN, when using a noise window ending 50 s before the P rival time. A noise window that overlaps the precursory time window may reduce the amplitude of the observed precursors, down-weighting seismograms with large-amplitude precursors. This effect is negligible, given that the amplitude of the noise on a single trace is up to 10 times greater than that of the precursors. Thus, we use a 140-s noise window ending 5 s before PKKPbc and a 15-s signal window starting at the PKKPbc onset time. It is also possible for the stack to be biased by an anomalously large reference phase (possibly resulting from focusing effects); this was avoided by assigning a maximum weight of 7 to each individual trace. Although the choice of noise window and weighting scheme can influence the absolute level of the observed precursors, the relative amplitude of the PKKPbc precursors with range was independent of the choice of windowing.
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    • . A model of CMB topography could not be found that fit our observations within their error bounds over the entire distance range, giving rise to the possibility of additional sources of scattering. Thus, limits were placed on the model parameters by consideration of models that matched the general character of the observations. Synthetics for λ < 7 km predict a precursory wave train that does not monotonically increase with time at shorter distance ranges, which is a result of the increased contribution of ab-to-ab scattering. Synthetics calculated for λ > 10 m concentrate the observed energy near the PKKPbc arrival.
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    • We thank the personnel from the IRIS-GSN stations for providing the data and specifically R. Benson for maintaining the FARM archive. This work benefited from the suggestions of B. Engdahl, two anonymous reviewers, and many co-workers and was supported by NSF grant EAR93-15060.


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