Abstract We show how to use a spreadsheet to calculate numerical solutions of the one-dimensional time-dependent heat-conduction equation. We find the spreadsheet to be a practical tool for numerical calculations, because the algorithms can be implemented simply and quickly without complicated programming, and the spreadsheet utilities can be used not only for graphics, printing, and file management, but also for advanced mathematical operations. We implement the explicit and the Crank-Nicholson forms of the finite-difference approximations and discuss the geological applications of both methods. We also show how to adjust these two algorithms to a nonhomogeneous lithosphere in which the thermal properties (thermal conductivity, density, and radioactive heat generation) change from the upper crust to the lower crust and to the mantle. The solution is presented in a way that can fit any spreadsheet (Lotus-123, Quattro-Pro, Excel). In addition, a Quattro-Pro program with macros that calculate and display the thermal evolution of the lithosphere after a thermal perturbation is enclosed in an appendix.
[1]
G. Smith,et al.
Numerical Solution of Partial Differential Equations: Finite Difference Methods
,
1978
.
[2]
J. C. Jaeger,et al.
Conduction of Heat in Solids
,
1952
.
[3]
David R. Kincaid,et al.
Numerical mathematics and computing
,
1980
.
[4]
H. Day,et al.
Controls on the Apparent Thermal and Baric Structure of Mountain Belts
,
1987,
The Journal of Geology.
[5]
Alan Bruce Thompson,et al.
Pressure—Temperature—Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental Crust
,
1984
.
[6]
Simon M. Peacock,et al.
Creation and preservation of subduction-related inverted metamorphic gradients
,
1987
.
[7]
W. Press,et al.
Numerical Recipes: The Art of Scientific Computing
,
1987
.
[8]
John G. Sclater,et al.
Continental Margin Subsidence and Heat Flow: Important Parameters in Formation of Petroleum Hydrocarbons
,
1980
.