[ghsc-seminars] GHSC Seminar: TOMORROW, Tuesday, July 21st, 10-11 am -- Fred Pollitz, USGS

[Rigler, Erin (Josh) Joshua]

Fred Pollitz
U.S. Geological Survey
Earthquake Science Center

Tuesday, July 21st, 2020
10-11am
(Mountain Time)
Virtual Seminar

Join Microsoft Teams Meeting<https://teams.microsoft.com/l/meetup-join/19%3ameeting_YzMwODFlZDktYmY1OS00YmM0LTk3ZGUtMTA0Y2ExYmUxNGRm%40thread.v2/0?context=%7b%22Tid%22%3a%220693b5ba-4b18-4d7b-9341-f32f400a5494%22%2c%22Oid%22%3a%22d6329638-ca90-40d3-9ece-4674ffcbda6a%22%2c%22MessageId%22%3a%220%22%7d>


Title:
Coseismic slip and afterslip of the 2020 Magna, Utah, earthquake

Abstract:

The 2020 Magna, Utah, earthquake produced observable crustal deformation over a ∼ 100 km2 area around the southeast margin of Great Salt Lake, but it did not produce any surface rupture. To obtain a detailed picture of the fault slip, we combine strong mo- tion seismic waveforms with GPS static offsets and Interferometric Synthetic Aperture Radar (InSAR) observations to obtain kinematic and static slip models of the event. We sample the regional seismic wavefield with 3-component records from 68 stations of the University of Utah Seismograph Stations network. We find that coseismic slip and afterslip, with predominantly normal slip, distributed on a shallowly west-dipping plane, possibly augmented by afterslip on a steeply northeast-dipping plane, best fits the joint dataset. The west-dipping plane locates near previously inferred sources of interseismic creep at depth. Hence the earthquake may have occurred on the downdip extension of the Wasatch fault and activated further slip (afterslip) at shallow depth east of the hypocenter. This inferred afterslip may have driven the vigorous aftershock activity that was concentrated east of  the hypocenter.


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Thank you,
GHSC Seminar Committee

Francis Rengers - frengers at usgs.gov
Josh Rigler - erigler at usgs.gov
Oliver Boyd - olboyd at usgs.gov
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