Abstract
IN solids, the rates of kinetic processes such as volume diffusion and order–disorder transitions are extremely sensitive to temperature. At room temperatures they are so slow that crystalline solids normally preserve a substantial degree of thermodynamic disequilibrium over very long periods (> 109 yr in some cases). At sufficiently high temperatures, on the other hand, some processes go so fast that a continuously varying state of equilibrium may be maintained as the temperature changes. When a solid cools steadily a transition occurs from the one state (continuous equilibrium) to the other (false equilibrium) in the neighbourhood of the closure temperature, which is defined below. Here I present a simple quantitative argument relating closure temperature to the cooling rate and kinetic parameters of a given kinetic system (see refs 1–6 for related work).
This is a preview of subscription content, access via your institution
Access options
Subscribe to this journal
Receive 51 print issues and online access
$199.00 per year
only $3.90 per issue
Buy this article
- Purchase on Springer Link
- Instant access to full article PDF
Prices may be subject to local taxes which are calculated during checkout
Similar content being viewed by others
References
Dodson, M. H., Contr. Miner. Petrol., 40, 259–276 (1973).
Wagner, G. A., and Reimer, G. M., Earth planet. Sci. Lett., 14, 263–268 (1972).
Seifert, F., and Virgo, D., Science, 188, 1107–1109 (1975).
Lasaga, A. C., and Richardson, S., EOS, Trans. Am. Geophys. Un., 56, 459 (1975).
Sykes, C., and Evans, H., J. Inst. Metals, 58, 255–280 (1936).
Burke, J., and Stuckey, D., Phil. Mag., 31, 1063–1080 (1975).
Crank, J., Mathematics of Diffusion (Oxford, Clarendon Press, 1956)
Goldstein, J. I., and Short, J. M., Geochim. cosmochim. Acta, 31, 1001–1023 (1967).
Seifert, F., and Virgo, D., Yb. Carnegie Inst. Wash., 73, 405–411 (1974).
Jäger, E., Niggli, E., and Wenk, E., Beitr. geol. Karte Schweiz, N.F. 134 (1967).
Clark, S. P., and Jäger, E., Am. J. Sci., 267, 1143–1160 (1969).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
DODSON, M. Kinetic processes and thermal history of slowly cooling solids. Nature 259, 551–553 (1976). https://doi.org/10.1038/259551a0
Received:
Accepted:
Issue Date:
DOI: https://doi.org/10.1038/259551a0
This article is cited by
-
Were oxygen isotopes of hydrothermally altered minerals just elevated by the 18O-enriched water? Theoretical inversion with thermodynamics and kinetics
Mineralogy and Petrology (2024)
-
Effect of pressure on closure temperature of a trace element in cooling petrological systems
Contributions to Mineralogy and Petrology (2017)
-
Thermal metamorphism of the Arunachal Himalaya, India: Raman thermometry and thermochronological constraints on the tectono-thermal evolution
International Journal of Earth Sciences (2013)
-
Diffusion modeling as a tool for constraining timescales of evolution of metamorphic rocks
Mineralogy and Petrology (2006)
-
Diagenetic-metallogenic ages of pyritic cherts and their implications in Mojiang nickel-gold deposit in Yunnan Province, China
Chinese Science Bulletin (2001)
Comments
By submitting a comment you agree to abide by our Terms and Community Guidelines. If you find something abusive or that does not comply with our terms or guidelines please flag it as inappropriate.