<HashMap><database>biostudies-literature</database><scores/><additional><submitter>Li Z</submitter><funding>European Research Council</funding><pagination>2787</pagination><full_dataset_link>https://www.ebi.ac.uk/biostudies/studies/S-EPMC9120171</full_dataset_link><repository>biostudies-literature</repository><omics_type>Unknown</omics_type><volume>13(1)</volume><pubmed_abstract>The lowermost mantle right above the core-mantle boundary is highly heterogeneous containing multiple poorly understood seismic features. The smallest but most extreme heterogeneities yet observed are 'Ultra-Low Velocity Zones' (ULVZ). We exploit seismic shear waves that diffract along the core-mantle boundary to provide new insight into these enigmatic structures. We measure a rare core-diffracted signal refracted by a ULVZ at the base of the Hawaiian mantle plume at unprecedentedly high frequencies. This signal shows remarkably longer time delays at higher compared to lower frequencies, indicating a pronounced internal variability inside the ULVZ. Utilizing the latest computational advances in 3D waveform modeling, here we show that we are able to model this high-frequency signal and con</pubmed_abstract><journal>Nature communications</journal><pubmed_title>Kilometer-scale structure on the core-mantle boundary near Hawaii.</pubmed_title><pmcid>PMC9120171</pmcid><funding_grant_id>No.804071-ZoomDeep</funding_grant_id><funding_grant_id>804071</funding_grant_id><pubmed_authors>Li Z</pubmed_authors><pubmed_authors>Cottaar S</pubmed_authors><pubmed_authors>Leng K</pubmed_authors><pubmed_authors>Jenkins J</pubmed_authors></additional><is_claimable>false</is_claimable><name>Kilometer-scale structure on the core-mantle boundary near Hawaii.</name><description>The lowermost mantle right above the core-mantle boundary is highly heterogeneous containing multiple poorly understood seismic features. The smallest but most extreme heterogeneities yet observed are 'Ultra-Low Velocity Zones' (ULVZ). We exploit seismic shear waves that diffract along the core-mantle boundary to provide new insight into these enigmatic structures. We measure a rare core-diffracted signal refracted by a ULVZ at the base of the Hawaiian mantle plume at unprecedentedly high frequencies. This signal shows remarkably longer time delays at higher compared to lower frequencies, indicating a pronounced internal variability inside the ULVZ. Utilizing the latest computational advances in 3D waveform modeling, here we show that we are able to model this high-frequency signal and con</description><dates><release>2022-01-01T00:00:00Z</release><publication>2022 May</publication><modification>2025-04-22T00:29:52.859Z</modification><creation>2025-04-05T19:34:09.077Z</creation></dates><accession>S-EPMC9120171</accession><cross_references><pubmed>35589765</pubmed><doi>10.1038/s41467-022-30502-5</doi></cross_references></HashMap>