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Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas.

Research output: Contribution to Journal/MagazineJournal article

Published

Standard

Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas. / Phillips, J. C.; Lane, S. J.; Lejeune, A.-M. et al.
In: Bulletin of Volcanology, Vol. 57, No. 4, 1995, p. 263-268.

Research output: Contribution to Journal/MagazineJournal article

Harvard

Phillips, JC, Lane, SJ, Lejeune, A-M & Hilton, M 1995, 'Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas.', Bulletin of Volcanology, vol. 57, no. 4, pp. 263-268. https://doi.org/10.1007/BF00265425

APA

Phillips, J. C., Lane, S. J., Lejeune, A-M., & Hilton, M. (1995). Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas. Bulletin of Volcanology, 57(4), 263-268. https://doi.org/10.1007/BF00265425

Vancouver

Phillips JC, Lane SJ, Lejeune A-M, Hilton M. Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas. Bulletin of Volcanology. 1995;57(4):263-268. doi: 10.1007/BF00265425

Author

Phillips, J. C. ; Lane, S. J. ; Lejeune, A.-M. et al. / Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas. In: Bulletin of Volcanology. 1995 ; Vol. 57, No. 4. pp. 263-268.

Bibtex

@article{7708c1182bd3411e80ea4bb4d1fae0d1,
title = "Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas.",
abstract = "Solutions of gum rosin and acetone reproduce the volatile- and temperature-dependent viscosity, together with the phase behaviour, of hydrated magmas. A range of experimental exsolution conditions was investigated, including the variation of supersaturation, rate of decompression, solution temperature and volatile content. Degassing processes were controlled by the formation of an exsolution interface above a supersaturated liquid. The end-products ranged from a mildly degassed liquid to a solid foam, which preserved strained vesicles. Solutions of gum rosin and acetone are proposed as a suitable analogue system with which to study magma degassing processes.",
author = "Phillips, {J. C.} and Lane, {S. J.} and A.-M. Lejeune and M. Hilton",
year = "1995",
doi = "10.1007/BF00265425",
language = "English",
volume = "57",
pages = "263--268",
journal = "Bulletin of Volcanology",
issn = "1432-0819",
publisher = "Springer-Verlag",
number = "4",

}

RIS

TY - JOUR

T1 - Gum rosin–acetone system as an analogue to the degassing behaviour of hydrated magmas.

AU - Phillips, J. C.

AU - Lane, S. J.

AU - Lejeune, A.-M.

AU - Hilton, M.

PY - 1995

Y1 - 1995

N2 - Solutions of gum rosin and acetone reproduce the volatile- and temperature-dependent viscosity, together with the phase behaviour, of hydrated magmas. A range of experimental exsolution conditions was investigated, including the variation of supersaturation, rate of decompression, solution temperature and volatile content. Degassing processes were controlled by the formation of an exsolution interface above a supersaturated liquid. The end-products ranged from a mildly degassed liquid to a solid foam, which preserved strained vesicles. Solutions of gum rosin and acetone are proposed as a suitable analogue system with which to study magma degassing processes.

AB - Solutions of gum rosin and acetone reproduce the volatile- and temperature-dependent viscosity, together with the phase behaviour, of hydrated magmas. A range of experimental exsolution conditions was investigated, including the variation of supersaturation, rate of decompression, solution temperature and volatile content. Degassing processes were controlled by the formation of an exsolution interface above a supersaturated liquid. The end-products ranged from a mildly degassed liquid to a solid foam, which preserved strained vesicles. Solutions of gum rosin and acetone are proposed as a suitable analogue system with which to study magma degassing processes.

U2 - 10.1007/BF00265425

DO - 10.1007/BF00265425

M3 - Journal article

VL - 57

SP - 263

EP - 268

JO - Bulletin of Volcanology

JF - Bulletin of Volcanology

SN - 1432-0819

IS - 4

ER -