Seth A. Stein
Northwestern University, Evanston, IL
Activity
2023
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A MORE REALISTIC FAULTING MODEL IMPROVES EARTHQUAKE FORECASTS
T219 What’s in a Fault? Fault Structure, Deformation Mechanisms, and Why Fault Zones Matter to Society: In Honor of James P. EvansWednesday, 18 October 20238:00 AM - 12:00 PM315 / 316
2022
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WHEN’S THE NEXT EARTHQUAKE? A MORE REALISTIC MODEL OF EARTHQUAKE RECURRENCE AND PROBABILITY
106 GSA Geophysics and Geodynamics Division 50th Anniversary Special Session and George Woollard Lecture IIMonday, 10 October 20221:30 PM - 5:30 PM205
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WHY DO EARTHQUAKE HAZARD MAPS PREDICT HIGHER SHAKING THAN OBSERVED?
72 GSA Geophysics and Geodynamics Division 50th Anniversary Special Session and George Woollard Lecture IMonday, 10 October 20228:00 AM - 12:00 PM205
2021
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COMPARING ONSHORE AND OFFSHORE VOLUMES OF LARGE IGNEOUS PROVINCES ASSOCIATED WITH PASSIVE CONTINENTAL MARGINS
T102 Rifts, Rifted Margins, Backarcs, and Spreading Ridges: Understanding Extensional Processes across Tectonic Settings and Time Scales IIMonday, 11 October 20211:30 PM - 5:30 PMB115/B116 (Hybrid Room)
2020
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SHOULD ALL OF NEPAL BE TREATED AS HAVING THE SAME EARTHQUAKE HAZARD?
T6 The Multidisciplinary Approach of the Seismotectonics as a Key Tool to Expand Horizons on Faulting Process Understanding and to Address Effective Seismic Hazard Assessment IMonday, 26 October 20201:30 PM - 5:30 PMMeeting Rooms
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NEOPROTEROZOIC SEDIMENTATION IN THE LAURENTIAN MIDCONTINENT: DETRITAL ZIRCON PROVENANCE OF THE JACOBSVILLE SANDSTONE, LAKE SUPERIOR BASIN, USA AND CANADA
2 Insights into Processes of Proterozoic Crustal Growth, Modification, and Stabilization in the North-Central U.S. Continental InteriorMonday, 18 May 20208:00 AM - 12:00 PMFrench River Room 1
2018
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DETRITAL ZIRCON U-PB GEOCHRONOLOGY OF THE NEOPROTEROZOIC JACOBSVILLE SANDSTONE ON THE EASTERN END OF LAKE SUPERIOR, ONTARIO, CANADA
264 D31. Precambrian Geology (Posters)Wednesday, 7 November 20189:00 AM - 6:30 PMHalls J-K
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DOES LONG-TERM FAULT MEMORY CONTRIBUTE TO THE SPACE-TIME VARIABILITY OF CONTINENTAL INTRAPLATE SEISMICITY?
T208 Earthquakes and Deformation in Eastern North America and Other Continental Interiors: What We Know, What We Don’t, What We Think, and Which Is Which?Tuesday, 6 November 20181:30 PM - 5:30 PMRoom 238-239
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A SEISMIC EXPERIMENT TO INVESTIGATE MAJOR CRUSTAL-SCALE STRUCTURES IN EASTERN KENTUCKY AND TENNESSEE
T158 Beyond EarthScope in the Eastern U.S.—What We've Learned and What Needs Doing NextTuesday, 6 November 20188:00 AM - 12:00 PMRoom 238-239
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OPENING OF THE MIDCONTINENT RIFT DURING THE ASSEMBLY OF RODINIA
T91 Different Roads to Rodinia: Re-Analysis of the Geochronology and Tectonic Evolution of Precambrian Sedimentary and Crystalline Basement Terranes in Southeastern LaurentiaMonday, 5 November 20188:00 AM - 12:00 PMRoom 242
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IMPLICATIONS OF GEOCHEMICAL, PETROGRAPHIC AND STRATIGRAPHIC ANALYSES OF THE UPPER PORTAGE LAKE VOLCANICS FOR THE KEWEENAW FLOOD BASALTS
T119 Evolution of the Midcontinent Rift: A Window into Proterozoic Environments, a Repository of Minerals, and a Lesson in Rifting (Posters)Monday, 5 November 20189:00 AM - 6:30 PMHalls J-K
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PRECAMBRIAN RIFT SYSTEMS IN NORTH AMERICA COMPARED TO OTHER CONTINENTAL RIFTS AROUND THE WORLD
T16 Evolution of the Midcontinent Rift: A Window into Proterozoic Environments, a Repository of Minerals, and a Lesson in Rifting ISunday, 4 November 20188:00 AM - 12:00 PMRoom 242
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CRUSTAL CONTAMINATION IN THE TERMINAL STAGES OF THE KEWEENAWAN LARGE IGNEOUS PROVINCE: GEOCHEMICAL EVIDENCE FROM THE PORCUPINE MOUNTAINS
T16 Evolution of the Midcontinent Rift: A Window into Proterozoic Environments, a Repository of Minerals, and a Lesson in Rifting ISunday, 4 November 20188:00 AM - 12:00 PMRoom 242
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TERMINAL STAGES OF A DYING RIFT
T16 Evolution of the Midcontinent Rift: A Window into Proterozoic Environments, a Repository of Minerals, and a Lesson in Rifting ISunday, 4 November 20188:00 AM - 12:00 PMRoom 242