The ascent of felsic magmas in dykes

Nick Petford, John R. Lister, Ross C. Kerr

Research output: Contribution to Book/Report typesChapterResearchpeer-review

Abstract

The results of a thermal and fluid-dynamical analysis are presented that allow geologists to estimate the critical dyke or fracture width (wc) necessary for the transport of felsic magma through the crust without control by solidification. The principal geological variables required to estimate wc are the magmatic viscosity (μ), the density and temperature contrasts (Δρ{variant} and ΔT) between magma and country rock, and the height of ascent H. The results show that for typical values of μ and Δρ{variant}, and for transport distances of 20 to 30 km, the critical dyke width is constrained to lie between about 2 and 20 m. © 1994.
Original languageEnglish
Title of host publicationLITHOS
Pages161-168
Number of pages8
DOIs
Publication statusPublished - 1 Mar 1994

Publication series

NameLITHOS
Volume32

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dike
magma
solidification
country rock
viscosity
crust
fluid
temperature
analysis

Cite this

Petford, N., Lister, J. R., & Kerr, R. C. (1994). The ascent of felsic magmas in dykes. In LITHOS (pp. 161-168). (LITHOS; Vol. 32). https://doi.org/10.1016/0024-4937(94)90028-0
Petford, Nick ; Lister, John R. ; Kerr, Ross C. / The ascent of felsic magmas in dykes. LITHOS. 1994. pp. 161-168 (LITHOS).
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Petford, N, Lister, JR & Kerr, RC 1994, The ascent of felsic magmas in dykes. in LITHOS. LITHOS, vol. 32, pp. 161-168. https://doi.org/10.1016/0024-4937(94)90028-0

The ascent of felsic magmas in dykes. / Petford, Nick; Lister, John R.; Kerr, Ross C.

LITHOS. 1994. p. 161-168 (LITHOS; Vol. 32).

Research output: Contribution to Book/Report typesChapterResearchpeer-review

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AU - Lister, John R.

AU - Kerr, Ross C.

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N2 - The results of a thermal and fluid-dynamical analysis are presented that allow geologists to estimate the critical dyke or fracture width (wc) necessary for the transport of felsic magma through the crust without control by solidification. The principal geological variables required to estimate wc are the magmatic viscosity (μ), the density and temperature contrasts (Δρ{variant} and ΔT) between magma and country rock, and the height of ascent H. The results show that for typical values of μ and Δρ{variant}, and for transport distances of 20 to 30 km, the critical dyke width is constrained to lie between about 2 and 20 m. © 1994.

AB - The results of a thermal and fluid-dynamical analysis are presented that allow geologists to estimate the critical dyke or fracture width (wc) necessary for the transport of felsic magma through the crust without control by solidification. The principal geological variables required to estimate wc are the magmatic viscosity (μ), the density and temperature contrasts (Δρ{variant} and ΔT) between magma and country rock, and the height of ascent H. The results show that for typical values of μ and Δρ{variant}, and for transport distances of 20 to 30 km, the critical dyke width is constrained to lie between about 2 and 20 m. © 1994.

UR - http://www.mendeley.com/research/ascent-felsic-magmas-dykes

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DO - 10.1016/0024-4937(94)90028-0

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SN - 0024-4937

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Petford N, Lister JR, Kerr RC. The ascent of felsic magmas in dykes. In LITHOS. 1994. p. 161-168. (LITHOS). https://doi.org/10.1016/0024-4937(94)90028-0