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.


BIOMARKERS

Molecular Biopsy of Human Tumors

- a resource for Precision Medicine *

134 related articles for article (PubMed ID: 35918359)

  • 1. Sources of dehydration fluids underneath the Kamchatka arc.
    Shu Y; Nielsen SG; Le Roux V; Wörner G; Blusztajn J; Auro M
    Nat Commun; 2022 Aug; 13(1):4467. PubMed ID: 35918359
    [TBL] [Abstract][Full Text] [Related]  

  • 2. Molybdenum isotopes unmask slab dehydration and melting beneath the Mariana arc.
    Li HY; Zhao RP; Li J; Tamura Y; Spencer C; Stern RJ; Ryan JG; Xu YG
    Nat Commun; 2021 Oct; 12(1):6015. PubMed ID: 34650082
    [TBL] [Abstract][Full Text] [Related]  

  • 3. Melting of subducted slab dictates trace element recycling in global arcs.
    Li H; Hermann J; Zhang L
    Sci Adv; 2022 Jan; 8(2):eabh2166. PubMed ID: 35020421
    [TBL] [Abstract][Full Text] [Related]  

  • 4. Genesis of ultra-high-Ni olivine in high-Mg andesite lava triggered by seamount subduction.
    Nishizawa T; Nakamura H; Churikova T; Gordeychik B; Ishizuka O; Haraguchi S; Miyazaki T; Vaglarov BS; Chang Q; Hamada M; Kimura JI; Ueki K; Toyama C; Nakao A; Iwamori H
    Sci Rep; 2017 Sep; 7(1):11515. PubMed ID: 28912418
    [TBL] [Abstract][Full Text] [Related]  

  • 5. Arc-like magmas generated by mélange-peridotite interaction in the mantle wedge.
    Codillo EA; Le Roux V; Marschall HR
    Nat Commun; 2018 Jul; 9(1):2864. PubMed ID: 30030428
    [TBL] [Abstract][Full Text] [Related]  

  • 6. Geochemical evidence for mélange melting in global arcs.
    Nielsen SG; Marschall HR
    Sci Adv; 2017 Apr; 3(4):e1602402. PubMed ID: 28435882
    [TBL] [Abstract][Full Text] [Related]  

  • 7. Crustal thickness control on Sr/Y signatures of recent arc magmas: an Earth scale perspective.
    Chiaradia M
    Sci Rep; 2015 Jan; 5():8115. PubMed ID: 25631193
    [TBL] [Abstract][Full Text] [Related]  

  • 8. Variable water input controls evolution of the Lesser Antilles volcanic arc.
    Cooper GF; Macpherson CG; Blundy JD; Maunder B; Allen RW; Goes S; Collier JS; Bie L; Harmon N; Hicks SP; Iveson AA; Prytulak J; Rietbrock A; Rychert CA; Davidson JP;
    Nature; 2020 Jun; 582(7813):525-529. PubMed ID: 32581382
    [TBL] [Abstract][Full Text] [Related]  

  • 9. U-Th Isotopes in Arc Magmas: Implications for Element Transfer from the Subducted Crust.
    Hawkesworth CJ; Turner SP; McDermott F; Peate DW; van Calsteren P
    Science; 1997 Apr; 276(5312):551-5. PubMed ID: 9110968
    [TBL] [Abstract][Full Text] [Related]  

  • 10. Subduction of fracture zones controls mantle melting and geochemical signature above slabs.
    Manea VC; Leeman WP; Gerya T; Manea M; Zhu G
    Nat Commun; 2014 Oct; 5():5095. PubMed ID: 25342158
    [TBL] [Abstract][Full Text] [Related]  

  • 11. Louisville seamount subduction and its implication on mantle flow beneath the central Tonga-Kermadec arc.
    Timm C; Bassett D; Graham IJ; Leybourne MI; de Ronde CE; Woodhead J; Layton-Matthews D; Watts AB
    Nat Commun; 2013; 4():1720. PubMed ID: 23591887
    [TBL] [Abstract][Full Text] [Related]  

  • 12. Slab melting boosts the mantle wedge contribution to Li-rich magmas.
    Schettino E; González-Pérez I; Marchesi C; González-Jiménez JM; Grégoire M; Tilhac R; Gervilla F; Blanco-Quintero IF; Corgne A; Schilling ME
    Sci Rep; 2024 Jul; 14(1):15168. PubMed ID: 38956121
    [TBL] [Abstract][Full Text] [Related]  

  • 13. Mafic slab melt contributions to Proterozoic massif-type anorthosites.
    Keller DS; Lee CA; Peck WH; Monteleone BD; Martin C; Vervoort JD; Bolge L
    Sci Adv; 2024 Aug; 10(33):eadn3976. PubMed ID: 39141730
    [TBL] [Abstract][Full Text] [Related]  

  • 14. Tracing halogen and B cycling in subduction zones based on obducted, subducted and forearc serpentinites of the Dominican Republic.
    Pagé L; Hattori K
    Sci Rep; 2017 Dec; 7(1):17776. PubMed ID: 29259321
    [TBL] [Abstract][Full Text] [Related]  

  • 15. Separation of supercritical slab-fluids to form aqueous fluid and melt components in subduction zone magmatism.
    Kawamoto T; Kanzaki M; Mibe K; Matsukage KN; Ono S
    Proc Natl Acad Sci U S A; 2012 Nov; 109(46):18695-700. PubMed ID: 23112158
    [TBL] [Abstract][Full Text] [Related]  

  • 16. Kinematic variables and water transport control the formation and location of arc volcanoes.
    Grove TL; Till CB; Lev E; Chatterjee N; Médard E
    Nature; 2009 Jun; 459(7247):694-7. PubMed ID: 19494913
    [TBL] [Abstract][Full Text] [Related]  

  • 17. Water-sulfur-rich, oxidised adakite magmas are likely porphyry copper progenitors.
    Leong TSJ; Mavrogenes JA; Arculus RJ
    Sci Rep; 2023 Mar; 13(1):5078. PubMed ID: 36977810
    [TBL] [Abstract][Full Text] [Related]  

  • 18. Nitrogen recycling at the Costa Rican subduction zone: The role of incoming plate structure.
    Lee H; Fischer TP; de Moor JM; Sharp ZD; Takahata N; Sano Y
    Sci Rep; 2017 Oct; 7(1):13933. PubMed ID: 29066787
    [TBL] [Abstract][Full Text] [Related]  

  • 19. Experimental production of K-rich metasomes through sediment recycling at the slab-mantle interface in the fore-arc.
    Gülmez F; Prelević D; Förster MW; Buhre S; Günther J
    Sci Rep; 2023 Nov; 13(1):19608. PubMed ID: 37949895
    [TBL] [Abstract][Full Text] [Related]  

  • 20. The subducted component in island arc lavas: constraints from Be isotopes and B-Be systematics.
    Morris JD; Leeman WP; Tera F
    Nature; 1990 Mar; 344(6261):31-6. PubMed ID: 18278019
    [TBL] [Abstract][Full Text] [Related]  

    [Next]    [New Search]
    of 7.