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

Clifford A. Kaye; John C. Maxwell; Peter Verrall

doi:10.1029/tr034i006p00953

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

Clifford A. Kaye·John C. Maxwell·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?

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Clifford A. Kaye, John C. Maxwell, Peter Verrall. 2014-08-18. Discussion of “expansion and increase in permeability of carbonate rocks on heating”. https://doi.org/10.1029/tr034i006p00953

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