These tools will no longer be maintained as of December 31, 2024. Archived website can be found here. PubMed4Hh GitHub repository can be found here. Contact NLM Customer Service if you have questions.
409 related articles for article (PubMed ID: 15772658)
1. Subducted banded iron formations as a source of ultralow-velocity zones at the core-mantle boundary. Dobson DP; Brodholt JP Nature; 2005 Mar; 434(7031):371-4. PubMed ID: 15772658 [TBL] [Abstract][Full Text] [Related]
2. Origins of ultralow velocity zones through slab-derived metallic melt. Liu J; Li J; Hrubiak R; Smith JS Proc Natl Acad Sci U S A; 2016 May; 113(20):5547-51. PubMed ID: 27143719 [TBL] [Abstract][Full Text] [Related]
3. Superionic iron hydride shapes ultralow-velocity zones at Earth's core-mantle boundary. Zhang Y; Wang W; Li Y; Wu Z Proc Natl Acad Sci U S A; 2024 Aug; 121(35):e2406386121. PubMed ID: 39163332 [TBL] [Abstract][Full Text] [Related]
4. Seismological constraints on a possible plume root at the core-mantle boundary. Rost S; Garnero EJ; Williams Q; Manga M Nature; 2005 Jun; 435(7042):666-9. PubMed ID: 15931220 [TBL] [Abstract][Full Text] [Related]
5. Hydrogen-bearing iron peroxide and the origin of ultralow-velocity zones. Liu J; Hu Q; Young Kim D; Wu Z; Wang W; Xiao Y; Chow P; Meng Y; Prakapenka VB; Mao HK; Mao WL Nature; 2017 Nov; 551(7681):494-497. PubMed ID: 29168804 [TBL] [Abstract][Full Text] [Related]
6. Iron-rich post-perovskite and the origin of ultralow-velocity zones. Mao WL; Mao HK; Sturhahn W; Zhao J; Prakapenka VB; Meng Y; Shu J; Fei Y; Hemley RJ Science; 2006 Apr; 312(5773):564-5. PubMed ID: 16645091 [TBL] [Abstract][Full Text] [Related]
7. Globally distributed subducted materials along the Earth's core-mantle boundary: Implications for ultralow velocity zones. Hansen SE; Garnero EJ; Li M; Shim SH; Rost S Sci Adv; 2023 Apr; 9(14):eadd4838. PubMed ID: 37018398 [TBL] [Abstract][Full Text] [Related]
8. Seismic detection of folded, subducted lithosphere at the core-mantle boundary. Hutko AR; Lay T; Garnero EJ; Revenaugh J Nature; 2006 May; 441(7091):333-6. PubMed ID: 16710418 [TBL] [Abstract][Full Text] [Related]
9. Iron-silica interaction at extreme conditions and the electrically conducting layer at the base of Earth's mantle. Dubrovinsky L; Dubrovinskaia N; Langenhorst F; Dobson D; Rubie D; Gessmann C; Abrikosov IA; Johansson B; Baykov VI; Vitos L; Le Bihan T; Crichton WA; Dmitriev V; Weber HP Nature; 2003 Mar; 422(6927):58-61. PubMed ID: 12621431 [TBL] [Abstract][Full Text] [Related]
10. Extensive iron-water exchange at Earth's core-mantle boundary can explain seismic anomalies. Kawano K; Nishi M; Kuwahara H; Kakizawa S; Inoue T; Kondo T Nat Commun; 2024 Oct; 15(1):8701. PubMed ID: 39406711 [TBL] [Abstract][Full Text] [Related]
11. Chemical interaction of Fe and Al(2)O3 as a source of heterogeneity at the Earth's core-mantle boundary. Dubrovinsky L; Annersten H; Dubrovinskaia N; Westman F; Harryson H; Fabrichnaya O; Carlson S Nature; 2001 Aug; 412(6846):527-9. PubMed ID: 11484050 [TBL] [Abstract][Full Text] [Related]
12. The influence of a chemical boundary layer on the fixity, spacing and lifetime of mantle plumes. Jellinek AM; Manga M Nature; 2002 Aug; 418(6899):760-3. PubMed ID: 12181562 [TBL] [Abstract][Full Text] [Related]
13. Earth's Core-Mantle Boundary: Results of Experiments at High Pressures and Temperatures. Knittle E; Jeanloz R Science; 1991 Mar; 251(5000):1438-43. PubMed ID: 17779437 [TBL] [Abstract][Full Text] [Related]
14. Efficacy of the post-perovskite phase as an explanation for lowermost-mantle seismic properties. Wookey J; Stackhouse S; Kendall JM; Brodholt J; Price GD Nature; 2005 Dec; 438(7070):1004-7. PubMed ID: 16355222 [TBL] [Abstract][Full Text] [Related]
15. GEOPHYSICS: Core Takes a Page From the Sea Floor. Kerr RA Science; 2000 Nov; 290(5495):1274b-5b. PubMed ID: 17787225 [TBL] [Abstract][Full Text] [Related]
17. Mantle shear-wave tomography and the fate of subducted slabs. Grand SP Philos Trans A Math Phys Eng Sci; 2002 Nov; 360(1800):2475-91. PubMed ID: 12460476 [TBL] [Abstract][Full Text] [Related]
18. Ocean productivity before about 1.9 Gyr ago limited by phosphorus adsorption onto iron oxides. Bjerrum CJ; Canfield DE Nature; 2002 May; 417(6885):159-62. PubMed ID: 12000956 [TBL] [Abstract][Full Text] [Related]
20. Seismic detection of rigid zones at the top of the core. Rost S; Revenaugh J Science; 2001 Nov; 294(5548):1911-4. PubMed ID: 11729313 [TBL] [Abstract][Full Text] [Related] [Next] [New Search]