Manuscripts In Review
Peer-Reviewed Publications
[16] Salditch, L., Gallahue, M.M., Stein, S., Neely, J.S., Abrahamson, N., Hough, S.E. (2024). Why do seismic hazard maps worldwide appear to overpredict historical intensity observations? Science Advances (Accepted)
[15] Neely, J.S., Salditch, L., Spencer, B.D., Stein S. (2024) The Generalized Long-Term Fault Memory model and applications to paleoseismic records. Bulletin of the Seismological Society of America. doi:10.1785/0120230185
[14] Lucas, M.C, Hough, S.E., Stein, S., Salditch, L., Gallahue, M.M., Neely, J.S., Abrahamson, N. (2023) Uncertainties in intensity-based earthquake magnitude estimates. Seismological Research Letters. doi:10.1785/0220230030
[13] Gallahue, M.M., Salditch, L., Lucas, M.C., Neely, J.S., Stein S., Abrahamson, N., Hough, S.E. (2023), Exploring the effect of minimum magnitude on California seismic hazard models. Seismica 2(1). doi:10.26443/seismica.v2i1.212
[12] Neely, J.S., Salditch, L., Spencer, B.D., Stein S. (2023), A more realistic model for the probability of large earthquakes. Bulletin of the Seismological Society of America 113(2). doi:10.1785/0120220083.
[11] Gallahue, M.M., Salditch, L., Lucas, M.C., Neely, J.S., Stein S., Abrahamson, N., Williams, T., Hough, S.E. (2022), A study on the effect of site response on California seismic hazard map assessment. Frontiers in Earth Science 10. doi:10.3389/feart.2022.931340
[10] Neely, J.S., Stein S. (2021), Why do continental normal fault earthquakes have smaller maximum magnitudes? Tectonophysics 809. doi:10.1016/j.tecto.2021.228854
[9] Hough, S.E., Page, M., Salditch, L., Gallahue, M.M., Lucas, M.C., Neely, J.S., Stein, S. (2021), Revisiting California’s past great earthquakes and long-term earthquake rate, Bulletin of the Seismological Society of America111(1), 356-370. doi:10.1785/0120200253
[8] Salditch, L., Gallahue, M.M., Lucas, M.C, Neely, J.S., Hough, S.E., Stein, S. (2020), California Historical Intensity Mapping Project (CHIMP): A consistently reinterpreted dataset of seismic intensities for the past 162 years and implications for seismic hazard map, Seismological Research Letters 91(5), 2631-2650. doi:10.1785/0220200065
[7] Neely, J.S., Stein, S., Spencer, B.D. (2020), Large uncertainties in earthquake stress-drop estimates and their tectonic consequences, Seismological Research Letters 91(4), 2320-2323. doi:10.1785/0220200004
[6] Salditch, L., Stein, S., Neely, J.S., Spencer, B.D., Brooks, E.M., Agnon, A., Liu, M. (2020), Earthquake supercycles and Long-Term Fault Memory, Tectonophysics 774. doi:10.1016/j.tecto.2019.228289
[5] Neely, J.S., Huang, Y., Fan, W. (2019), Earthquake rupture characteristics along a developing transform boundary, Geophysical Journal International 219(2), 1237-1252. doi:10.1093/gji/ggz357
[4] Brooks, E.M., Neely, J.S., Stein, S., Spencer, B.D., Salditch, L. (2019), Assessments of the performance of the 2017 one-year seismic hazard forecast for the central and eastern United States via simulated earthquake shaking data, Seismological Research Letters 90(3), 1155-1167. doi:10.1785/0220190007
[3] Neely, J.S., Stein, S., Merino, M., Adams, J. (2018), Have we seen the largest earthquakes in eastern North America? Physics of the Earth and Planetary Interiors 284, 17-27. doi:10.1016/j.pepi.2018.09.005
[2] Salditch, L., Hough, S.E., Stein, S., Spencer, B.D., Brooks, E.M., Neely, J.S., Lucas, M.C. (2018), The 1952 Kern County, California earthquake: A case study of issues in the analysis of historical intensity data for estimation of source parameters. Physics of the Earth and Planetary Interiors 283, 140-151. doi:10.1016/j.pepi.2018.08.007
[1] Neely, J.S., Furlong, K.P. (2018), Evidence of displacement-driven maturation along the San Cristobal Trough transform plate boundary. Earth and Planetary Science Letters 485, 88–98. doi:10.1016/j.epsl.2017.12.044