Vedran Lekic, Ph.D.
Affiliations: | 2009 | University of California, Berkeley, Berkeley, CA, United States |
Area:
GeophysicsGoogle:
"Vedran Lekic"Mean distance: 2084.92
Parents
Sign in to add mentorBarbara Romanowicz | grad student | 2009 | UC Berkeley | |
(Inferring the elastic structure of the Earth's mantle using the spectral element method.) |
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Publications
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Samuel H, Drilleau M, Rivoldini A, et al. (2023) Geophysical evidence for an enriched molten silicate layer above Mars's core. Nature. 622: 712-717 |
Irving JCE, Lekić V, Durán C, et al. (2023) First observations of core-transiting seismic phases on Mars. Proceedings of the National Academy of Sciences of the United States of America. 120: e2217090120 |
Li J, Beghein C, McLennan SM, et al. (2022) Constraints on the martian crust away from the InSight landing site. Nature Communications. 13: 7950 |
Huang Q, Schmerr NC, King SD, et al. (2022) Seismic detection of a deep mantle discontinuity within Mars by InSight. Proceedings of the National Academy of Sciences of the United States of America. 119: e2204474119 |
Stähler SC, Khan A, Banerdt WB, et al. (2021) Seismic detection of the martian core. Science (New York, N.Y.). 373: 443-448 |
Knapmeyer-Endrun B, Panning MP, Bissig F, et al. (2021) Thickness and structure of the martian crust from InSight seismic data. Science (New York, N.Y.). 373: 438-443 |
Khan A, Ceylan S, van Driel M, et al. (2021) Upper mantle structure of Mars from InSight seismic data. Science (New York, N.Y.). 373: 434-438 |
Magrini F, Boschi L, Gualtieri L, et al. (2021) Rayleigh-wave attenuation across the conterminous United States in the microseism frequency band. Scientific Reports. 11: 10149 |
Kim D, Lekić V, Ménard B, et al. (2020) Sequencing seismograms: A panoptic view of scattering in the core-mantle boundary region. Science (New York, N.Y.). 368: 1223-1228 |
Cunningham E, Lekic V. (2020) Constraining Properties of Sedimentary Strata Using Receiver Functions: An Example from the Atlantic Coastal Plain of the Southeastern United States Bulletin of the Seismological Society of America. 110: 519-533 |