Discussion of “expansion and increase in permeability of carbonate rocks on heating”
Eos, Transactions, American Geophysical Union
By: Clifford A. Kaye, John C. Maxwell, and Peter Verrall
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Abstract
Maxwell and Verrall's interesting study raises a thought. If limestones expand on heating and thereby receive a permanent set, as this paper demonstrates, do we not have here a means of determining the maximum temperature to which a particular limestone was ever subjected and indirectly thereby its maximum depth of burial or other geothermal events in its history?
Suggested Citation
Kaye, C., Maxwell, J.C., and Verrall, P., 1953, Discussion of “expansion and increase in permeability of carbonate rocks on heating”: Eos, Transactions, American Geophysical Union, v. 34, no. 6, p. 953-954, https://doi.org/10.1029/TR034i006p00953.
ISSN: 2324-9250 (online)
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Discussion of “expansion and increase in permeability of carbonate rocks on heating” |
| Series title | Eos, Transactions, American Geophysical Union |
| DOI | 10.1029/TR034i006p00953 |
| Volume | 34 |
| Issue | 6 |
| Publication Date | August 18, 2014 |
| Year Published | 1953 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 2 p. |
| First page | 953 |
| Last page | 954 |