An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems

Chongbin Zhao; Bruce E. Hobbs; Alison Ord

doi:10.1007/978-3-540-89743-9_7

An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems

Chongbin Zhao, Bruce E. Hobbs, Alison Ord

Research output: Chapter in Book/Conference paper › Chapter › peer-review

Abstract

Consideration of the effects of magma ascending and solidification is important to the further understanding of ore body formation and mineralization in the crust of the Earth. Although various possible fundamental mechanisms of magma ascending in the crust are proposed (Johnson and Pollard, 1973, Marsh 1982, Lister and Kerr 1991, Rubin 1995, Weinberg 1996, Bons et al. 2001), the development of numerical algorithms for simulating the proposed magma ascending mechanisms is still under-developed. For example, continuum-mechanics-based numerical methods have encountered serious difficulties in simulating the random generation and propagation of hydro-fractured cracks, the magma flow within these cracks, the solidification of the ascending magma due to heat losses to the surrounding rocks, and so forth.

Original language	English
Title of host publication	Fundamentals of Computational Geoscience
Subtitle of host publication	Numerical Methods and Algorithms
Editors	Chongbin Zhao, Bruce Hobbs, Alison Ord, Alison Ord
Publisher	Springer
Pages	153-173
Number of pages	21
ISBN (Print)	9783540897422
DOIs	https://doi.org/10.1007/978-3-540-89743-9_7
Publication status	Published - 7 May 2009

Publication series

Name	Lecture Notes in Earth Sciences
Volume	122
ISSN (Print)	0930-0317

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10.1007/978-3-540-89743-9_7

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Zhao, C., Hobbs, B. E., & Ord, A. (2009). An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems. In C. Zhao, B. Hobbs, A. Ord, & A. Ord (Eds.), Fundamentals of Computational Geoscience: Numerical Methods and Algorithms (pp. 153-173). (Lecture Notes in Earth Sciences; Vol. 122). Springer. https://doi.org/10.1007/978-3-540-89743-9_7

Zhao, Chongbin ; Hobbs, Bruce E. ; Ord, Alison. / An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems. Fundamentals of Computational Geoscience: Numerical Methods and Algorithms. editor / Chongbin Zhao ; Bruce Hobbs ; Alison Ord ; Alison Ord. Springer, 2009. pp. 153-173 (Lecture Notes in Earth Sciences).

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abstract = "Consideration of the effects of magma ascending and solidification is important to the further understanding of ore body formation and mineralization in the crust of the Earth. Although various possible fundamental mechanisms of magma ascending in the crust are proposed (Johnson and Pollard, 1973, Marsh 1982, Lister and Kerr 1991, Rubin 1995, Weinberg 1996, Bons et al. 2001), the development of numerical algorithms for simulating the proposed magma ascending mechanisms is still under-developed. For example, continuum-mechanics-based numerical methods have encountered serious difficulties in simulating the random generation and propagation of hydro-fractured cracks, the magma flow within these cracks, the solidification of the ascending magma due to heat losses to the surrounding rocks, and so forth.",

author = "Chongbin Zhao and Hobbs, {Bruce E.} and Alison Ord",

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Zhao, C, Hobbs, BE & Ord, A 2009, An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems. in C Zhao, B Hobbs, A Ord & A Ord (eds), Fundamentals of Computational Geoscience: Numerical Methods and Algorithms. Lecture Notes in Earth Sciences, vol. 122, Springer, pp. 153-173. https://doi.org/10.1007/978-3-540-89743-9_7

An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems. / Zhao, Chongbin; Hobbs, Bruce E.; Ord, Alison.
Fundamentals of Computational Geoscience: Numerical Methods and Algorithms. ed. / Chongbin Zhao; Bruce Hobbs; Alison Ord; Alison Ord. Springer, 2009. p. 153-173 (Lecture Notes in Earth Sciences; Vol. 122).

Research output: Chapter in Book/Conference paper › Chapter › peer-review

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AB - Consideration of the effects of magma ascending and solidification is important to the further understanding of ore body formation and mineralization in the crust of the Earth. Although various possible fundamental mechanisms of magma ascending in the crust are proposed (Johnson and Pollard, 1973, Marsh 1982, Lister and Kerr 1991, Rubin 1995, Weinberg 1996, Bons et al. 2001), the development of numerical algorithms for simulating the proposed magma ascending mechanisms is still under-developed. For example, continuum-mechanics-based numerical methods have encountered serious difficulties in simulating the random generation and propagation of hydro-fractured cracks, the magma flow within these cracks, the solidification of the ascending magma due to heat losses to the surrounding rocks, and so forth.

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An equivalent source algorithm for simulating thermal and chemical effects of intruded magma solidification problems

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