Veins in clay-rich aquitards as records of deformation and fluid-flow events in northern Switzerland
Abstract
The Jurassic clay-rich aquitard sequence underlying the Swiss Molasse Basin is locally penetrated by unusually frequent veins consisting of calcite ± celestite, in particular in the Schlattingen-1 and Oftringen drill cores. The veins are linked to extensional brittle structures, with shear senses ranging between dip-slip and strike-slip. Deformation triggered transient and localised events of fluid flow within the aquitard followed by sealing of...
Paper Details
Title
Veins in clay-rich aquitards as records of deformation and fluid-flow events in northern Switzerland
Published Date
Aug 1, 2018
Journal
Volume
95
Pages
57 - 70
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