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Moitra, P., Albadi, A., Tatsch, A., Santra, P. (2025) Flow‐ and Fracture‐Driven Bubble Throat Growth Rates and Dynamic Permeability in Crystallizing Magma. Geochemistry, Geophysics, Geosystems, 26 (2). doi:10.1029/2024gc011932

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Reference TypeJournal (article/letter/editorial)
TitleFlow‐ and Fracture‐Driven Bubble Throat Growth Rates and Dynamic Permeability in Crystallizing Magma
JournalGeochemistry, Geophysics, Geosystems
AuthorsMoitra, P.Author
Albadi, A.Author
Tatsch, A.Author
Santra, P.Author
Year2025 (February)Volume26
Issue2
PublisherAmerican Geophysical Union (AGU)
DOIdoi:10.1029/2024gc011932Search in ResearchGate
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Mindat Ref. ID17978956Long-form Identifiermindat:1:5:17978956:4
GUID0
Full ReferenceMoitra, P., Albadi, A., Tatsch, A., Santra, P. (2025) Flow‐ and Fracture‐Driven Bubble Throat Growth Rates and Dynamic Permeability in Crystallizing Magma. Geochemistry, Geophysics, Geosystems, 26 (2). doi:10.1029/2024gc011932
Plain TextMoitra, P., Albadi, A., Tatsch, A., Santra, P. (2025) Flow‐ and Fracture‐Driven Bubble Throat Growth Rates and Dynamic Permeability in Crystallizing Magma. Geochemistry, Geophysics, Geosystems, 26 (2). doi:10.1029/2024gc011932
In(2025, February) Geochemistry, Geophysics, Geosystems Vol. 26 (2). Wiley

References Listed

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Not Yet Imported: Physics of Fluids - journal-article : 10.1063/1.869942

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Not Yet Imported: - journal-article : 10.1122/1.548848

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Mezger T. G. (2006) The rheology handbook: For users of rotational and oscillatory rheometers
Moitra P. Albadi A. Tatsch A. &Santra P.(2025).Data for flow and fracture driven bubble throat growth rates and dynamic permeability in crystallizing magma.https://doi.org/10.25422/azu.data.27169284
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Mueller S. (2010) Proceedings of the Royal Society of London A: Mathematical, Physical and Engineering Sciences The rheology of suspensions of solid particles
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Not Yet Imported: Frontiers in Physics - journal-article : 10.3389/fphy.2015.00060

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Sable J. E. (2009) Eruption mechanisms during the climax of the Tarawera 1886 basaltic Plinian eruption inferred from microtextural characteristics‐of the deposits , 129
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