Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm
Thesis advisor: John E. Ebel === Large magnitude offshore passive margin earthquakes are rare, making small magnitude events (M < 4) the predominant data available to study the mechanisms of seismicity along passive margins. This study is focused on a swarm of events (M2.1-M3.9) that occurred fro...
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ndltd-BOSTON-oai-dlib.bc.edu-bc-ir_1067142019-05-10T07:35:23Z Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm Napoli, Vanessa J. Thesis advisor: John E. Ebel Text thesis 2016 Boston College English electronic application/pdf Large magnitude offshore passive margin earthquakes are rare, making small magnitude events (M < 4) the predominant data available to study the mechanisms of seismicity along passive margins. This study is focused on a swarm of events (M2.1-M3.9) that occurred from 2012-2013 located in the Gulf of Maine (GM) along the Atlantic Passive Margin (APM) shelf break, a region with previously minimal recorded seismic activity. Relative locations were calculated for the earthquakes of the GM swarm and a moment tensor inversion method was used to calculate focal mechanisms for the two largest events in the swarm. The results of the relative location method constrained a fault orientation to a strike of 243° ± 3° and a dip of 25° ± 3°. The focal mechanisms for the two largest events were determined to be oblique normal faults with steeply dipping planes at depths between 12-18 km. For the largest event (M3.9), the strike is 235° ± 1°, with a dip of 77.7° ± .8° and a rake of -116.5° ± 3°, and for the second largest event (M3.7) the strike is 259° ± 3°, with a dip of 78° ± 2° and a rake of -58.8° ± 7°. By mapping the spatial extent of the relative hypocenters, I infer a potential fault size of 2.7 km by 2.4 km. If this entire area were to rupture at once in the future, an earthquake of M4.9-M5.0 could occur, a magnitude not large enough to be tsunamigenic in the GM. Based on Gutenberg-Richter relations from the eastern APM, if a M7 can occur in the GM, its estimated mean repeat time is 2,120-22,800 years, and it could be tsunamigenic depending on the event’s proximity to the continental slope. Focal Mechanism Gulf of Maine Passive Margin Relative Location Seismology Tsunami Copyright is held by the author, with all rights reserved, unless otherwise noted. Thesis (MS) — Boston College, 2016. Submitted to: Boston College. Graduate School of Arts and Sciences. Discipline: Earth and Environmental Sciences. http://hdl.handle.net/2345/bc-ir:106714 |
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Focal Mechanism Gulf of Maine Passive Margin Relative Location Seismology Tsunami |
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Focal Mechanism Gulf of Maine Passive Margin Relative Location Seismology Tsunami Napoli, Vanessa J. Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
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Thesis advisor: John E. Ebel === Large magnitude offshore passive margin earthquakes are rare, making small magnitude events (M < 4) the predominant data available to study the mechanisms of seismicity along passive margins. This study is focused on a swarm of events (M2.1-M3.9) that occurred from 2012-2013 located in the Gulf of Maine (GM) along the Atlantic Passive Margin (APM) shelf break, a region with previously minimal recorded seismic activity. Relative locations were calculated for the earthquakes of the GM swarm and a moment tensor inversion method was used to calculate focal mechanisms for the two largest events in the swarm. The results of the relative location method constrained a fault orientation to a strike of 243° ± 3° and a dip of 25° ± 3°. The focal mechanisms for the two largest events were determined to be oblique normal faults with steeply dipping planes at depths between 12-18 km. For the largest event (M3.9), the strike is 235° ± 1°, with a dip of 77.7° ± .8° and a rake of -116.5° ± 3°, and for the second largest event (M3.7) the strike is 259° ± 3°, with a dip of 78° ± 2° and a rake of -58.8° ± 7°. By mapping the spatial extent of the relative hypocenters, I infer a potential fault size of 2.7 km by 2.4 km. If this entire area were to rupture at once in the future, an earthquake of M4.9-M5.0 could occur, a magnitude not large enough to be tsunamigenic in the GM. Based on Gutenberg-Richter relations from the eastern APM, if a M7 can occur in the GM, its estimated mean repeat time is 2,120-22,800 years, and it could be tsunamigenic depending on the event’s proximity to the continental slope. === Thesis (MS) — Boston College, 2016. === Submitted to: Boston College. Graduate School of Arts and Sciences. === Discipline: Earth and Environmental Sciences. |
author |
Napoli, Vanessa J. |
author_facet |
Napoli, Vanessa J. |
author_sort |
Napoli, Vanessa J. |
title |
Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
title_short |
Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
title_full |
Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
title_fullStr |
Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
title_full_unstemmed |
Relative Location Analysis and Moment Tensor Inversion for the 2012 Gulf of Maine Earthquake Swarm |
title_sort |
relative location analysis and moment tensor inversion for the 2012 gulf of maine earthquake swarm |
publisher |
Boston College |
publishDate |
2016 |
url |
http://hdl.handle.net/2345/bc-ir:106714 |
work_keys_str_mv |
AT napolivanessaj relativelocationanalysisandmomenttensorinversionforthe2012gulfofmaineearthquakeswarm |
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1719079228924755968 |