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Intra-eruptive trachyte-phonolite transition: natural evidences and experimental constraints on the role of crystal mushes
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Integrated petrologic, geochemical and experimental investigation of intraplate alkaline magmas at Dunedin Volcano: constraints on mantle sources, differentiation trends and magmatic processes
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Table S2 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Table S2 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Table S1 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Table S1 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Table S3 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Supplementary material from "Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures" ...
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Table S3 from Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures ...
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Supplementary material from "Transient to stationary radon ( 220 Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures" ...
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Transient to stationary radon ((220)Rn) emissions from a phonolitic rock exposed to subvolcanic temperatures
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Increase in radon emission due to rock failure: an experimental study
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In: ISSN: 0094-8276 ; EISSN: 1944-8007 ; Geophysical Research Letters ; https://hal.archives-ouvertes.fr/hal-00724843 ; Geophysical Research Letters, American Geophysical Union, 2011, pp.L14304. ⟨10.1029/2011GL047962⟩ (2011)
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