MM
Member Since 2019
Molly Margaret Gallahue
Graduate Student, Northwestern University
AGU Research
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Biases in Ground-Motion to Intensity Conversion Equations (GMICE): Causes and Updated Methodologies
THE VALUE OF MACROSEISMIC INTENSITY DATA: FROM EARTHQUAKE SOURCE CHARACTERIZATION TO GROUND MOTION AND SEISMIC HAZARD ESTIMATION AND TESTING I ORAL
seismology | 14 december 2023
Molly M. Gallahue, Norman A. Abrahamson
Ground-motion to intensity conversion equations (GMICE) allow for conversion between ground-motion amplitude and shaking intensity. The current method...
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How Well Can Macroseismic Intensities Constrain Moment Magnitude?
THE VALUE OF MACROSEISMIC INTENSITY DATA: FROM EARTHQUAKE SOURCE CHARACTERIZATION TO GROUND MOTION AND SEISMIC HAZARD ESTIMATION AND TESTING I ORAL
seismology | 14 december 2023
Madeleine C Lucas, Susan E. Hough, Seth Stein, Lea...
Macroseismic data are valuable, and often required, to constrain earthquake source parameters for historical (pre-instrumental) earthquakes. Current m...
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Why does PSHA overpredict historically observed shaking data?
SEISMOLOGY CONTRIBUTIONS: EARTHQUAKE GROUND MOTIONS AND ENGINEERING SEISMOLOGY III ORAL
seismology | 15 december 2022
Leah Salditch, Molly M. Gallahue, James S. Neely,...
Probabilistic seismic hazard assessments (PSHA) based on current practice consistently appear to overpredict historically observed shaking data. Compa...
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Re-evaluating Ground Motion Intensity Conversion Equations for California and Implications for Hazard Map Assessment
SEISMOLOGY CONTRIBUTIONS: EARTHQUAKE GROUND MOTIONS AND ENGINEERING SEISMOLOGY III ORAL
seismology | 15 december 2022
Molly M. Gallahue, Norman A. Abrahamson
Ground-motion intensity conversion equations (GMICE) are used to describe the relationship between ground-motion amplitude and shaking intensity. GMIC...
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Insights into Continental Rifting and Oceanic Crust Formation from Integrating Data from Passive Margins and Continental Rifts
OCEANIC AND CONTINENTAL EXTENSIONAL TECTONICS II ORAL
tectonophysics | 13 december 2022
Carol A. Stein, Seth Stein, Molly M. Gallahue, Re...
Integrating marine geophysical data from passive margins with on-land data from continental rifts yields insights into the processes by which continen...
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Exploring site effects in probabilistic seismic hazard maps
SEISMOLOGY CONTRIBUTIONS: EARTHQUAKE GROUND MOTIONS AND ENGINEERING SEISMOLOGY I ORAL
seismology | 13 december 2021
Molly M. Gallahue, Leah Salditch, Madeleine C Luc...
Probabilistic seismic hazard assessment (PSHA) generates one of the most important products produced by the seismological community for earthquake haz...
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Assessment of seismic hazard map performance for California through comparison with historical shaking data
STUDENT ENGAGEMENT TO ENHANCE DEVELOPMENT: OUTSTANDING STUDENT PRESENTATION AWARD WINNERS FROM FALL MEETING 2019 VII ELIGHTNING
union | 15 december 2020
Molly M. Gallahue, Leah Salditch, Madeleine C Luc...
Probabilistic seismic hazard assessments are important for earthquake hazard mitigation. They forecast levels of earthquake shaking that should be exc...
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How much melt forms in continental rifting and where does it go?
WHERE IS THE MELT DURING THE EVOLUTION OF CONTINENTAL RIFTING? I
tectonophysics | 14 december 2020
Molly M. Gallahue, Seth Stein, Carol A. Stein, Do...
The rifting and breakup of continents leads to the initiation of seafloor spreading and eventual formation of passive margins. Some margins, termed ma...
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