Abstract When slip at shallow depth occurs during large subduction zone thrust events,Pwave energy enters the water layer and establishespwP, the reverberating waves called “water bounces” that followpP. For water depths ≥5–6 km (i.e., near the trench) above the shallow slip,pwPmanifests in a strong ~10‐s period ringing that can persist for minutes into the teleseismicPwave coda at all azimuths. Deeper slip can generate shorter‐periodpwPringing at trenchward azimuths. At large distances,Pcodawindows have several‐minute‐long intervals free of secondary arrivals. We consider rmsPcoda/rmsPamplitude ratios at distances from 80° to 120° as a potential proxy for occurrence of shallow slip for 39MW7.5+ megathrust earthquakes from 1990 to 2016 with estimated slip distributions. Ratios for the 15‐ to 7‐s‐period band have a strong bimodal distribution, with higher averagePcoda/Pamplitudes observed for ruptures with slip extending to shallow depth. 
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                            Imaging an Enigmatic Paleovalley with Passive Seismic Methods (Unaweep Canyon, Colorado, United States)
                        
                    
    
            Abstract High-resolution passive seismic imaging of shallow subsurface structures is often challenged by the scarcity of coherent body-wave energy in ambient noise recorded at surface stations. We show that the autocorrelation (AC) of teleseismic P-wave coda extracted from just one month of continuous recording at 5 Hz geophones can overcome this limitation. We apply this method to investigate the longitudinal subsurface bedrock structure of Unaweep Canyon—a paleovalley in western Colorado (United States) with complex evolution. Both fluvial and glacial processes have been proposed to explain the canyon’s genesis and morphology. The teleseismic P-wave coda AC retrieves zero-offset reflections from the shallow (200–500 m depth) basement interface at 120 stations along a 5 km long profile. In addition, we invert interferometrically retrieved surface-wave dispersion for the shear-wave structure of the sedimentary fill. Combined interpretation of these results and other geophysical and well data suggests an overdeepened basement geometry most consistent with glacial processes. 
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                            - Award ID(s):
- 1849623
- PAR ID:
- 10435832
- Date Published:
- Journal Name:
- The Seismic Record
- Volume:
- 3
- Issue:
- 2
- ISSN:
- 2694-4006
- Page Range / eLocation ID:
- 116 to 124
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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