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?
| 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 |
| Year Published | 1953 |
| Language | English |
| Publisher | American Geophysical Union |
| Description | 2 p. |
| First page | 953 |
| Last page | 954 |
| Google Analytic Metrics | Metrics page |