The Depth of Fractures and Active Ground‐Water Flow in a Clayey Till Plain in Southwestern Ontario
- 1 May 1991
- journal article
- Published by Wiley in Groundwater
- Vol. 29 (3) , 405-417
- https://doi.org/10.1111/j.1745-6584.1991.tb00531.x
Abstract
No abstract availableKeywords
This publication has 6 references indexed in Scilit:
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- Fracture permeability and groundwater flow in clayey till near Saskatoon, SaskatchewanCanadian Geotechnical Journal, 1986
- Origin, age and movement of pore water in argillaceous Quaternary deposits at four sites in southwestern OntarioJournal of Hydrology, 1981
- The Chalk groundwater tritium anomaly — A possible explanationJournal of Hydrology, 1975
- Isotope HydrologyPublished by Elsevier ,1972
- Effect of groundwater levels on stress history of the St. Clair clay till depositCanadian Geotechnical Journal, 1970