2019•AGUFMRequires access

Thermal-Hydrological Models Consistent with Low Effective Porosity for Subseafloor Transport in the Upper Crust, Eastern Flank of the Juan de Fuca Ridge

T. S. Weathers, A. T. Fisher, Philip H. Stauffer, Carl W. Gable

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Key concepts: Geology, Ridge, Crust, Flank, Upper crust, Mid-ocean ridge, Thermal, Seismology

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Thermal-Hydrological Models Consistent with Low Effective Porosity for Subseafloor Transport in the Upper Crust, Eastern Flank of the Juan de Fuca Ridge — Research Paper | ScholarLens