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155 related items for PubMed ID: 31636209
1. Metallic iron limits silicate hydration in Earth's transition zone. Zhu F, Li J, Liu J, Dong J, Liu Z. Proc Natl Acad Sci U S A; 2019 Nov 05; 116(45):22526-22530. PubMed ID: 31636209 [Abstract] [Full Text] [Related]
5. Water content in the transition zone from electrical conductivity of wadsleyite and ringwoodite. Huang X, Xu Y, Karato S. Nature; 2005 Apr 07; 434(7034):746-9. PubMed ID: 15815625 [Abstract] [Full Text] [Related]
7. Global electromagnetic induction constraints on transition-zone water content variations. Kelbert A, Schultz A, Egbert G. Nature; 2009 Aug 20; 460(7258):1003-6. PubMed ID: 19693081 [Abstract] [Full Text] [Related]
9. A relatively dry mantle transition zone revealed by geomagnetic diurnal variations. Zhang H, Egbert GD, Huang Q. Sci Adv; 2022 Aug 05; 8(31):eabo3293. PubMed ID: 35921405 [Abstract] [Full Text] [Related]
10. Hydration-reduced lattice thermal conductivity of olivine in Earth's upper mantle. Chang YY, Hsieh WP, Tan E, Chen J. Proc Natl Acad Sci U S A; 2017 Apr 18; 114(16):4078-4081. PubMed ID: 28377520 [Abstract] [Full Text] [Related]
11. Constraining composition and temperature variations in the mantle transition zone. Zhou WY, Hao M, Zhang JS, Chen B, Wang R, Schmandt B. Nat Commun; 2022 Mar 01; 13(1):1094. PubMed ID: 35232983 [Abstract] [Full Text] [Related]
12. Evidence for the stability of ultrahydrous stishovite in Earth's lower mantle. Lin Y, Hu Q, Meng Y, Walter M, Mao HK. Proc Natl Acad Sci U S A; 2020 Jan 07; 117(1):184-189. PubMed ID: 31843935 [Abstract] [Full Text] [Related]
13. Buoyant hydrous mantle plume from the mantle transition zone. Kuritani T, Xia QK, Kimura JI, Liu J, Shimizu K, Ushikubo T, Zhao D, Nakagawa M, Yoshimura S. Sci Rep; 2019 Apr 25; 9(1):6549. PubMed ID: 31024064 [Abstract] [Full Text] [Related]
14. The pyrite-type high-pressure form of FeOOH. Nishi M, Kuwayama Y, Tsuchiya J, Tsuchiya T. Nature; 2017 Jul 13; 547(7662):205-208. PubMed ID: 28678774 [Abstract] [Full Text] [Related]
16. Large gem diamonds from metallic liquid in Earth's deep mantle. Smith EM, Shirey SB, Nestola F, Bullock ES, Wang J, Richardson SH, Wang W. Science; 2016 Dec 16; 354(6318):1403-1405. PubMed ID: 27980206 [Abstract] [Full Text] [Related]
17. Earth's interior. Dehydration melting at the top of the lower mantle. Schmandt B, Jacobsen SD, Becker TW, Liu Z, Dueker KG. Science; 2014 Jun 13; 344(6189):1265-8. PubMed ID: 24926016 [Abstract] [Full Text] [Related]
18. Water in Earth's Mantle: The Role of Nominally Anhydrous Minerals. Bell DR, Rossman GR. Science; 1992 Mar 13; 255(5050):1391-7. PubMed ID: 17801227 [Abstract] [Full Text] [Related]
19. The stability of FeHx and hydrogen transport at Earth's core mantle boundary. He Y, Kim DY, Struzhkin VV, Geballe ZM, Prakapenka V, Mao HK. Sci Bull (Beijing); 2023 Jul 30; 68(14):1567-1573. PubMed ID: 37355390 [Abstract] [Full Text] [Related]
20. Redox freezing and melting in the Earth's deep mantle resulting from carbon-iron redox coupling. Rohrbach A, Schmidt MW. Nature; 2011 Apr 14; 472(7342):209-12. PubMed ID: 21441908 [Abstract] [Full Text] [Related] Page: [Next] [New Search]