Skip to content

Formation and dynamics of magma reservoirs

Research output: Contribution to journalArticle

Standard

Formation and dynamics of magma reservoirs. / Sparks, Stephen; Annen, Catherine J; Blundy, Jon; Cashman, Katharine; Rust, Alison; Jackson, M D.

In: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, Vol. 377, No. 2139, 20190019, 07.01.2019.

Research output: Contribution to journalArticle

Harvard

Sparks, S, Annen, CJ, Blundy, J, Cashman, K, Rust, A & Jackson, MD 2019, 'Formation and dynamics of magma reservoirs', Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, vol. 377, no. 2139, 20190019. https://doi.org/10.1098/rsta.2018.0019

APA

Sparks, S., Annen, C. J., Blundy, J., Cashman, K., Rust, A., & Jackson, M. D. (2019). Formation and dynamics of magma reservoirs. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 377(2139), [20190019]. https://doi.org/10.1098/rsta.2018.0019

Vancouver

Sparks S, Annen CJ, Blundy J, Cashman K, Rust A, Jackson MD. Formation and dynamics of magma reservoirs. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 2019 Jan 7;377(2139). 20190019. https://doi.org/10.1098/rsta.2018.0019

Author

Sparks, Stephen ; Annen, Catherine J ; Blundy, Jon ; Cashman, Katharine ; Rust, Alison ; Jackson, M D. / Formation and dynamics of magma reservoirs. In: Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences. 2019 ; Vol. 377, No. 2139.

Bibtex

@article{cf8f0390a30044e68ba1d2d435a58b48,
title = "Formation and dynamics of magma reservoirs",
abstract = "The emerging concept of a magma reservoir is one in which regions containing melt extend from the source of magma generation to the surface. The reservoir may contain regions of very low fraction intergranular melt, partially molten rock (mush) and melt lenses (or magma chambers) containing high melt fraction eruptible magma, as well as pockets of exsolved magmatic fluids. The various parts of the system may be separated by sub-solidus rock or be connected and continuous. Magma reservoirs and their wall rocks span a vast array of rheological properties, covering as much as 25 orders of magnitude from high viscosity, sub-solidus crustal rocks to magmatic fluids. Timescales of processes within magma reservoirs range from very slow melt and fluid segregation within mush and magma chambers and deformation of surrounding host rocks to very rapid development of magma and fluid instability, transport and eruption. Developing a comprehensive model of these systems is a grand challenge that will require close collaboration between modellers, geophysicists, geochemists, geologists, volcanologists and petrologists.",
author = "Stephen Sparks and Annen, {Catherine J} and Jon Blundy and Katharine Cashman and Alison Rust and Jackson, {M D}",
year = "2019",
month = "1",
day = "7",
doi = "10.1098/rsta.2018.0019",
language = "English",
volume = "377",
journal = "Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences",
issn = "1364-503X",
publisher = "The Royal Society",
number = "2139",

}

RIS - suitable for import to EndNote

TY - JOUR

T1 - Formation and dynamics of magma reservoirs

AU - Sparks, Stephen

AU - Annen, Catherine J

AU - Blundy, Jon

AU - Cashman, Katharine

AU - Rust, Alison

AU - Jackson, M D

PY - 2019/1/7

Y1 - 2019/1/7

N2 - The emerging concept of a magma reservoir is one in which regions containing melt extend from the source of magma generation to the surface. The reservoir may contain regions of very low fraction intergranular melt, partially molten rock (mush) and melt lenses (or magma chambers) containing high melt fraction eruptible magma, as well as pockets of exsolved magmatic fluids. The various parts of the system may be separated by sub-solidus rock or be connected and continuous. Magma reservoirs and their wall rocks span a vast array of rheological properties, covering as much as 25 orders of magnitude from high viscosity, sub-solidus crustal rocks to magmatic fluids. Timescales of processes within magma reservoirs range from very slow melt and fluid segregation within mush and magma chambers and deformation of surrounding host rocks to very rapid development of magma and fluid instability, transport and eruption. Developing a comprehensive model of these systems is a grand challenge that will require close collaboration between modellers, geophysicists, geochemists, geologists, volcanologists and petrologists.

AB - The emerging concept of a magma reservoir is one in which regions containing melt extend from the source of magma generation to the surface. The reservoir may contain regions of very low fraction intergranular melt, partially molten rock (mush) and melt lenses (or magma chambers) containing high melt fraction eruptible magma, as well as pockets of exsolved magmatic fluids. The various parts of the system may be separated by sub-solidus rock or be connected and continuous. Magma reservoirs and their wall rocks span a vast array of rheological properties, covering as much as 25 orders of magnitude from high viscosity, sub-solidus crustal rocks to magmatic fluids. Timescales of processes within magma reservoirs range from very slow melt and fluid segregation within mush and magma chambers and deformation of surrounding host rocks to very rapid development of magma and fluid instability, transport and eruption. Developing a comprehensive model of these systems is a grand challenge that will require close collaboration between modellers, geophysicists, geochemists, geologists, volcanologists and petrologists.

U2 - 10.1098/rsta.2018.0019

DO - 10.1098/rsta.2018.0019

M3 - Article

VL - 377

JO - Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences

JF - Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences

SN - 1364-503X

IS - 2139

M1 - 20190019

ER -