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 *

324 related articles for article (PubMed ID: 14647379)

  • 1. Explosive volcanism may not be an inevitable consequence of magma fragmentation.
    Gonnermann HM; Manga M
    Nature; 2003 Nov; 426(6965):432-5. PubMed ID: 14647379
    [TBL] [Abstract][Full Text] [Related]  

  • 2. Magma heating by decompression-driven crystallization beneath andesite volcanoes.
    Blundy J; Cashman K; Humphreys M
    Nature; 2006 Sep; 443(7107):76-80. PubMed ID: 16957729
    [TBL] [Abstract][Full Text] [Related]  

  • 3. Strain-induced magma fragmentation in explosive eruptions.
    Papale P
    Nature; 1999 Feb; 397(6718):425-428. PubMed ID: 29667961
    [TBL] [Abstract][Full Text] [Related]  

  • 4. Thermal vesiculation during volcanic eruptions.
    Lavallée Y; Dingwell DB; Johnson JB; Cimarelli C; Hornby AJ; Kendrick JE; von Aulock FW; Kennedy BM; Andrews BJ; Wadsworth FB; Rhodes E; Chigna G
    Nature; 2015 Dec; 528(7583):544-7. PubMed ID: 26701056
    [TBL] [Abstract][Full Text] [Related]  

  • 5. Combined effusive-explosive silicic volcanism straddles the multiphase viscous-to-brittle transition.
    Wadsworth FB; Witcher T; Vossen CEJ; Hess KU; Unwin HE; Scheu B; Castro JM; Dingwell DB
    Nat Commun; 2018 Nov; 9(1):4696. PubMed ID: 30409969
    [TBL] [Abstract][Full Text] [Related]  

  • 6. Caldera-forming eruptions of mushy magma modulated by feedbacks between ascent rate, gas retention/loss and bubble/crystal framework interaction.
    Okumura S; L de Silva S; Nakamura M; Sasaki O
    Sci Rep; 2019 Nov; 9(1):15845. PubMed ID: 31676816
    [TBL] [Abstract][Full Text] [Related]  

  • 7. Explosive-effusive volcanic eruption transitions caused by sintering.
    Wadsworth FB; Llewellin EW; Vasseur J; Gardner JE; Tuffen H
    Sci Adv; 2020 Sep; 6(39):. PubMed ID: 32967820
    [TBL] [Abstract][Full Text] [Related]  

  • 8. New geochemical insights into volcanic degassing.
    Edmonds M
    Philos Trans A Math Phys Eng Sci; 2008 Dec; 366(1885):4559-79. PubMed ID: 18826919
    [TBL] [Abstract][Full Text] [Related]  

  • 9. In situ observation of the percolation threshold in multiphase magma analogues.
    Colombier M; Wadsworth FB; Scheu B; Vasseur J; Dobson KJ; Cáceres F; Allabar A; Marone F; Schlepütz CM; Dingwell DB
    Bull Volcanol; 2020; 82(4):32. PubMed ID: 32189822
    [TBL] [Abstract][Full Text] [Related]  

  • 10. Degassing during quiescence as a trigger of magma ascent and volcanic eruptions.
    Girona T; Costa F; Schubert G
    Sci Rep; 2015 Dec; 5():18212. PubMed ID: 26666396
    [TBL] [Abstract][Full Text] [Related]  

  • 11. The role of volatiles in magma chamber dynamics.
    Huppert HE; Woods AW
    Nature; 2002 Dec; 420(6915):493-5. PubMed ID: 12466839
    [TBL] [Abstract][Full Text] [Related]  

  • 12. Transition of Mount Etna lavas from a mantle-plume to an island-arc magmatic source.
    Schiano P; Clocchiatti R; Ottolini L; Busà T
    Nature; 2001 Aug; 412(6850):900-4. PubMed ID: 11528476
    [TBL] [Abstract][Full Text] [Related]  

  • 13. Transitions between explosive and effusive phases during the cataclysmic 2010 eruption of Merapi volcano, Java, Indonesia.
    Preece K; Gertisser R; Barclay J; Charbonnier SJ; Komorowski JC; Herd RA
    Bull Volcanol; 2016; 78(8):54. PubMed ID: 32355390
    [TBL] [Abstract][Full Text] [Related]  

  • 14. A compositional tipping point governing the mobilization and eruption style of rhyolitic magma.
    Di Genova D; Kolzenburg S; Wiesmaier S; Dallanave E; Neuville DR; Hess KU; Dingwell DB
    Nature; 2017 Dec; 552(7684):235-238. PubMed ID: 29239352
    [TBL] [Abstract][Full Text] [Related]  

  • 15. Shallow magma diversions during explosive diatreme-forming eruptions.
    Le Corvec N; Muirhead JD; White JDL
    Nat Commun; 2018 Apr; 9(1):1459. PubMed ID: 29654325
    [TBL] [Abstract][Full Text] [Related]  

  • 16. Forecasting Effusive Dynamics and Decompression Rates by Magmastatic Model at Open-vent Volcanoes.
    Ripepe M; Pistolesi M; Coppola D; Delle Donne D; Genco R; Lacanna G; Laiolo M; Marchetti E; Ulivieri G; Valade S
    Sci Rep; 2017 Jun; 7(1):3885. PubMed ID: 28634369
    [TBL] [Abstract][Full Text] [Related]  

  • 17. Bubble accumulation and its role in the evolution of magma reservoirs in the upper crust.
    Parmigiani A; Faroughi S; Huber C; Bachmann O; Su Y
    Nature; 2016 Apr; 532(7600):492-5. PubMed ID: 27074507
    [TBL] [Abstract][Full Text] [Related]  

  • 18. Redox evolution of a degassing magma rising to the surface.
    Burgisser A; Scaillet B
    Nature; 2007 Jan; 445(7124):194-7. PubMed ID: 17215841
    [TBL] [Abstract][Full Text] [Related]  

  • 19. Upward migration of Vesuvius magma chamber over the past 20,000 years.
    Scaillet B; Pichavant M; Cioni R
    Nature; 2008 Sep; 455(7210):216-9. PubMed ID: 18784723
    [TBL] [Abstract][Full Text] [Related]  

  • 20. Seismogenic lavas and explosive eruption forecasting.
    Lavallée Y; Meredith PG; Dingwell DB; Hess KU; Wassermann J; Cordonnier B; Gerik A; Kruhl JH
    Nature; 2008 May; 453(7194):507-10. PubMed ID: 18497822
    [TBL] [Abstract][Full Text] [Related]  

    [Next]    [New Search]
    of 17.