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Maréchal, Jean-Christophe, Perrochet, Pierre (2001) Theoretical relation between water flow rate in a vertical fracture and rock temperature in the surrounding massif. Earth and Planetary Science Letters, 194 (1) 213-219 doi:10.1016/s0012-821x(01)00551-9

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Reference TypeJournal (article/letter/editorial)
TitleTheoretical relation between water flow rate in a vertical fracture and rock temperature in the surrounding massif
JournalEarth and Planetary Science Letters
AuthorsMaréchal, Jean-ChristopheAuthor
Perrochet, PierreAuthor
Year2001 (December)Volume194
Issue1
PublisherElsevier BV
DOIdoi:10.1016/s0012-821x(01)00551-9Search in ResearchGate
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Mindat Ref. ID375604Long-form Identifiermindat:1:5:375604:5
GUID0
Full ReferenceMaréchal, Jean-Christophe, Perrochet, Pierre (2001) Theoretical relation between water flow rate in a vertical fracture and rock temperature in the surrounding massif. Earth and Planetary Science Letters, 194 (1) 213-219 doi:10.1016/s0012-821x(01)00551-9
Plain TextMaréchal, Jean-Christophe, Perrochet, Pierre (2001) Theoretical relation between water flow rate in a vertical fracture and rock temperature in the surrounding massif. Earth and Planetary Science Letters, 194 (1) 213-219 doi:10.1016/s0012-821x(01)00551-9
In(2001, December) Earth and Planetary Science Letters Vol. 194 (1) Elsevier BV

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