Discussion of “expansion and increase in permeability of carbonate rocks on heating”
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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 |
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