ORCID: https://orcid.org/0000-0002-0783-5065; Wadsworth, Fabian B.
ORCID: https://orcid.org/0000-0002-5341-208X; Dingwell, Donald B.
ORCID: https://orcid.org/0000-0002-3332-789X und Lavallée, Yan
ORCID: https://orcid.org/0000-0003-4766-5758
(2024):
Plug flow and brecciation in volcanic conduits can emerge from shear-induced crystal migration in otherwise Newtonian magmas.
In: Communications Earth & Environment, Bd. 5, 389
[PDF, 1MB]
Abstract
In the Earth, the flow of crystal-bearing magma is thought to be non-Newtonian and shear thinning, but the physical origin for this is poorly understood. We use hydro-granular theory to show that the decoupled migration of crystals toward conduit cores during magma ascent is a tenable microphysical mechanism for plug flow, emergent in an otherwise purely Newtonian crystal-bearing magma. We use a numerical conduit model to define the flow development length beyond which crystal migration dominates and strain localises near conduit margins. Applied to magma ascent scenarios, we show that this crystal-migration strain localisation only develops in high crystallinity magmas or magmas ascending in very narrow cracks/conduits. In all other scenarios, crystals do not contribute to non-Newtonian behaviour and such magmas are usually strictly Newtonian. The ascent of very crystal-rich dome magma could be associated with strain localisation and crystal depletion at the conduit margins, lubricating ascent through the crust.
| Dokumententyp: | Zeitschriftenartikel |
|---|---|
| EU Funded Grant Agreement Number: | 834225 |
| Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Mineralogie, Petrologie und Geochemie |
| Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
| URN: | urn:nbn:de:bvb:19-epub-127738-9 |
| ISSN: | 2662-4435 |
| Sprache: | Englisch |
| Dokumenten ID: | 127738 |
| Datum der Veröffentlichung auf Open Access LMU: | 17. Feb. 2026 07:39 |
| Letzte Änderungen: | 17. Feb. 2026 07:39 |
