Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake

On 8 August 2020, northwest North Carolina experienced an Mw 5.1 earthquake that caused damage to buildings and roads in the city of Sparta. A regional centroid moment tensor solution shows that the earthquake was the result of slip on a reverse fault with a minor strike-slip component. Interferomet...

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Main Authors: Charles W. Wicks, Jr., Jer-Ming Chiu
Format: Article
Language:English
Published: Seismological Society of America 2022-03-01
Series:The Seismic Record
Online Access:https://doi.org/10.1785/0320210044
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author Charles W. Wicks, Jr.
Jer-Ming Chiu
author_facet Charles W. Wicks, Jr.
Jer-Ming Chiu
author_sort Charles W. Wicks, Jr.
collection DOAJ
description On 8 August 2020, northwest North Carolina experienced an Mw 5.1 earthquake that caused damage to buildings and roads in the city of Sparta. A regional centroid moment tensor solution shows that the earthquake was the result of slip on a reverse fault with a minor strike-slip component. Interferometric Synthetic Aperture Radar (InSAR) data, from the Japan Aerospace Exploration Agency’s Advanced Land Observing Satellite #2 (ALOS2) satellite, reveal a deformation field that is more complex than expected from a single reverse fault earthquake. The data also reveal an apparent fault rupture at the Earth’s surface that caused damage to local roads. Modeling of the InSAR deformation field indicates the fault rupture is associated with a very shallow normal faulting event with an equivalent Mw of about 5.1 that overprinted the reverse fault deformation field and possibly occurred aseismically.
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spelling doaj.art-7835039fb4a54d669cee90468ce5337a2024-01-24T12:56:00ZengSeismological Society of AmericaThe Seismic Record2694-40062022-03-0121596710.1785/032021004421044Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina EarthquakeCharles W. Wicks, Jr.0https://orcid.org/0000-0002-0809-1328Jer-Ming Chiu1U.S. Geological Survey, Moffett Field, California, U.S.A.Center for Earthquake Research and Information, The University of Memphis, Memphis, Tennessee, U.S.A.On 8 August 2020, northwest North Carolina experienced an Mw 5.1 earthquake that caused damage to buildings and roads in the city of Sparta. A regional centroid moment tensor solution shows that the earthquake was the result of slip on a reverse fault with a minor strike-slip component. Interferometric Synthetic Aperture Radar (InSAR) data, from the Japan Aerospace Exploration Agency’s Advanced Land Observing Satellite #2 (ALOS2) satellite, reveal a deformation field that is more complex than expected from a single reverse fault earthquake. The data also reveal an apparent fault rupture at the Earth’s surface that caused damage to local roads. Modeling of the InSAR deformation field indicates the fault rupture is associated with a very shallow normal faulting event with an equivalent Mw of about 5.1 that overprinted the reverse fault deformation field and possibly occurred aseismically.https://doi.org/10.1785/0320210044
spellingShingle Charles W. Wicks, Jr.
Jer-Ming Chiu
Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
The Seismic Record
title Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
title_full Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
title_fullStr Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
title_full_unstemmed Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
title_short Surface Rupture on a Secondary Fault Associated with the 8 August 2020 Mw 5.1 Sparta North Carolina Earthquake
title_sort surface rupture on a secondary fault associated with the 8 august 2020 mw 5 1 sparta north carolina earthquake
url https://doi.org/10.1785/0320210044
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