125 related articles for article (PubMed ID: 29649871)
1. High-Pressure Evolution of Crystal Bonding Structures and Properties of FeOOH.
Lu C; Chen C
J Phys Chem Lett; 2018 May; 9(9):2181-2185. PubMed ID: 29649871
[TBL] [Abstract][Full Text] [Related]
2. The pyrite-type high-pressure form of FeOOH.
Nishi M; Kuwayama Y; Tsuchiya J; Tsuchiya T
Nature; 2017 Jul; 547(7662):205-208. PubMed ID: 28678774
[TBL] [Abstract][Full Text] [Related]
3. FeO2 and FeOOH under deep lower-mantle conditions and Earth's oxygen-hydrogen cycles.
Hu Q; Kim DY; Yang W; Yang L; Meng Y; Zhang L; Mao HK
Nature; 2016 Jun; 534(7606):241-4. PubMed ID: 27279220
[TBL] [Abstract][Full Text] [Related]
4. Mid-mantle water transportation implied by the electrical and seismic properties of ε-FeOOH.
Zhuang Y; Gan B; Cui Z; Tang R; Tao R; Hou M; Jiang G; Popescu C; Garbarino G; Zhang Y; Hu Q
Sci Bull (Beijing); 2022 Apr; 67(7):748-754. PubMed ID: 36546139
[TBL] [Abstract][Full Text] [Related]
5. Crystal structure, equation of state, and elasticity of phase H (MgSiO4H2) at Earth's lower mantle pressures.
Tsuchiya J; Mookherjee M
Sci Rep; 2015 Oct; 5():15534. PubMed ID: 26493639
[TBL] [Abstract][Full Text] [Related]
6. Exploring the structures and properties of nickel silicides at the pressures of the Earth's core.
Kong P; Wang J; Wang H; Ni Y; Wang H; Tang Y; Liu H; Chen Y
Phys Chem Chem Phys; 2021 Jul; 23(27):14671-14677. PubMed ID: 34223600
[TBL] [Abstract][Full Text] [Related]
7. Melting of iron at the physical conditions of the Earth's core.
Nguyen JH; Holmes NC
Nature; 2004 Jan; 427(6972):339-42. PubMed ID: 14737164
[TBL] [Abstract][Full Text] [Related]
8. High-pressure phase of brucite stable at Earth's mantle transition zone and lower mantle conditions.
Hermann A; Mookherjee M
Proc Natl Acad Sci U S A; 2016 Dec; 113(49):13971-13976. PubMed ID: 27872307
[TBL] [Abstract][Full Text] [Related]
9. Rare Helium-Bearing Compound FeO_{2}He Stabilized at Deep-Earth Conditions.
Zhang J; Lv J; Li H; Feng X; Lu C; Redfern SAT; Liu H; Chen C; Ma Y
Phys Rev Lett; 2018 Dec; 121(25):255703. PubMed ID: 30608845
[TBL] [Abstract][Full Text] [Related]
10. The influence of δ-(Al,Fe)OOH on seismic heterogeneities in Earth's lower mantle.
Ohira I; Jackson JM; Sturhahn W; Finkelstein GJ; Kawazoe T; Toellner TS; Suzuki A; Ohtani E
Sci Rep; 2021 Jun; 11(1):12036. PubMed ID: 34103572
[TBL] [Abstract][Full Text] [Related]
11. Iron-rich silicates in the Earth's D'' layer.
Mao WL; Meng Y; Shen G; Prakapenka VB; Campbell AJ; Heinz DL; Shu J; Caracas R; Cohen RE; Fei Y; Hemley RJ; Mao HK
Proc Natl Acad Sci U S A; 2005 Jul; 102(28):9751-3. PubMed ID: 15994226
[TBL] [Abstract][Full Text] [Related]
12. Pressure-induced structural change in MgSiO
Kono Y; Shibazaki Y; Kenney-Benson C; Wang Y; Shen G
Proc Natl Acad Sci U S A; 2018 Feb; 115(8):1742-1747. PubMed ID: 29432162
[TBL] [Abstract][Full Text] [Related]
13. High-pressure synthesis of ε-FeOOH from β-FeOOH and its application to the water oxidation catalyst.
Mukai K; Suzuki TM; Uyama T; Nonaka T; Morikawa T; Yamada I
RSC Adv; 2020 Dec; 10(73):44756-44767. PubMed ID: 35516263
[TBL] [Abstract][Full Text] [Related]
14. Radiative conductivity in the Earth's lower mantle.
Goncharov AF; Haugen BD; Struzhkin VV; Beck P; Jacobsen SD
Nature; 2008 Nov; 456(7219):231-4. PubMed ID: 19005553
[TBL] [Abstract][Full Text] [Related]
15. A doubling of the post-perovskite phase boundary and structure of the Earth's lowermost mantle.
Hernlund JW; Thomas C; Tackley PJ
Nature; 2005 Apr; 434(7035):882-6. PubMed ID: 15829961
[TBL] [Abstract][Full Text] [Related]
16. Pressure-stabilized divalent ozonide CaO
Wang Y; Xu M; Yang L; Yan B; Qin Q; Shao X; Zhang Y; Huang D; Lin X; Lv J; Zhang D; Gou H; Mao HK; Chen C; Ma Y
Nat Commun; 2020 Sep; 11(1):4702. PubMed ID: 32943627
[TBL] [Abstract][Full Text] [Related]
17. The elasticity of the MgSiO3 post-perovskite phase in the Earth's lowermost mantle.
Iitaka T; Hirose K; Kawamura K; Murakami M
Nature; 2004 Jul; 430(6998):442-5. PubMed ID: 15269765
[TBL] [Abstract][Full Text] [Related]
18. 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]
19. 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]
20. Magnetic Collapse in Transition Metal Oxides at High Pressure: Implications for the Earth.
Cohen RE; Mazin II; Isaak DG
Science; 1997 Jan; 275(5300):654-7. PubMed ID: 9005849
[TBL] [Abstract][Full Text] [Related]
[Next] [New Search]