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Passive Seismic ImagingStanford Exploration Project passive seismic imaging Brad Artman
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project passive imaging not event location structural imaging –reflection seismology: subsurface investigation from the time-delayed reflections of sound off of geologic variations. –passive imaging: with no application of controlled experimental sources, a relationship between a recorded transmission wavefield and reflection wavefields is required. requires: stationary seismometers, lots of disk space
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Passive Seismic ImagingStanford Exploration Project capitalizing on ambient noise earthquake arrivals ocean waves wind vibrations coupled with foundations cultural activity –vehicle and boat traffic –drilling noise –nearby seismic acquisition
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Passive Seismic ImagingStanford Exploration Project transmission wavefield time (s) depth (m) position(m)
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Passive Seismic ImagingStanford Exploration Project ambient noise r1r2 t r1r2
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Passive Seismic ImagingStanford Exploration Project ambient noise r1r2 t r1r2
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Passive Seismic ImagingStanford Exploration Project ambient noise r1r2 t r1r2
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Passive Seismic ImagingStanford Exploration Project ambient noise r1r2 t r1 r1 r1 r2 lag r1r2
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Passive Seismic ImagingStanford Exploration Project r1r2 t r1 r1 r1 r2 twt r1r2 ambient noise
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Passive Seismic ImagingStanford Exploration Project r1r2 t r1 r1 r1 r2 twt r1r2 ambient noise
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Passive Seismic ImagingStanford Exploration Project backscattered PP r1r2 t r1 r1 r1 r2 twt r1r2
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Passive Seismic ImagingStanford Exploration Project ambient noise r1r2 t r1 r1 r1 r2 lag twt r1r2
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Passive Seismic ImagingStanford Exploration Project 0 1200600 position(m) 20 25 30 time(s) 5 10 0200 100 lag(s) 0 0.1 0.3 400300 offset(m)
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Passive Seismic ImagingStanford Exploration Project 0 1200600 position(m) 20 25 30 time(s) 5 10 0 -100 200 100 lag(s) 0 0.1 0.3 offset(m) 300
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Passive Seismic ImagingStanford Exploration Project 0 1200600 position(m) 20 25 30 time(s) 5 10 0 -100-200 200 100 lag(s) 0 0.1 0.3 offset(m)
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Passive Seismic ImagingStanford Exploration Project 0 1200600 position(m) 20 25 30 time(s) 5 10 0 -100-200100 lag(s) 0 0.1 0.3 offset(m) -300 n long traces n short traces 2
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project The Sun as a Laboratory Acoustic Daylight Imaging via spectral factorization, Rickett SEP-100
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Passive Seismic ImagingStanford Exploration Project 2D Experiment 1 Receiver line
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Passive Seismic ImagingStanford Exploration Project Break Point?
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Passive Seismic ImagingStanford Exploration Project Whole Data Volume
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Passive Seismic ImagingStanford Exploration Project 8 Consecutive Lines
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Passive Seismic ImagingStanford Exploration Project 8 Spaced Lines
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project active synthetic reflection gather active migration
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Passive Seismic ImagingStanford Exploration Project passive synthetic correlated passive gather passive migration
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Passive Seismic ImagingStanford Exploration Project correlated passive gather passive migration passive synthetic
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project 2.5 D V app = V/cos ( )
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Passive Seismic ImagingStanford Exploration Project earthquake energy
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project Artman GeoServices
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Passive Seismic ImagingStanford Exploration Project Enlarged data set
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Passive Seismic ImagingStanford Exploration Project 5min Night
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Passive Seismic ImagingStanford Exploration Project 5min Night
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Passive Seismic ImagingStanford Exploration Project 10min Day
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Passive Seismic ImagingStanford Exploration Project passive imaging importance of 3D migration teleseisms breaking waves north sea reservoir
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Passive Seismic ImagingStanford Exploration Project Valhall one of the North sea giant fields partners Amerada Hess, Shell and Total reservoir highly porous chalk first production1982 field life2028
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Passive Seismic ImagingStanford Exploration Project Valhall Life of Field Seismic Permanent field wide seismic array installed at Valhall during 2003 –120 km seismic cables –2414 groups of 4C sensors –Covers 45sq km
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Passive Seismic ImagingStanford Exploration Project Oyo-Geospace cable
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Passive Seismic ImagingStanford Exploration Project operations
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Passive Seismic ImagingStanford Exploration Project Valhall data
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Passive Seismic ImagingStanford Exploration Project Valhall data 3 days, 2300 4C recievers 1.2 Tbytes
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Passive Seismic ImagingStanford Exploration Project Valhall data trace # Depth slice near 88m energy localized around rig moveout across traces suggests surface noise
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Passive Seismic ImagingStanford Exploration Project Valhall data Reflector? mono-freq. boat noise rig activity
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Passive Seismic ImagingStanford Exploration Project Valhall pipe cut normalization 4km 12km
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Passive Seismic ImagingStanford Exploration Project Valhall pipe cut image 4km 12km
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Passive Seismic ImagingStanford Exploration Project Valhall active seismic 4km 12km
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Passive Seismic ImagingStanford Exploration Project thank you
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Passive Seismic ImagingStanford Exploration Project Valhall pipe cut image 4km 12km
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