Clastic dykes in over-consolidated tills: evidence for subglacial hydrofracturing at Killiney Bay, eastern Ireland
- 1 November 1999
- journal article
- Published by Elsevier BV in Sedimentary Geology
- Vol. 129 (1-2), 111-126
- https://doi.org/10.1016/s0037-0738(99)00093-7
Abstract
No abstract availableKeywords
This publication has 33 references indexed in Scilit:
- Groundwater flow beneath ice sheets: Part II — Its impact on glacier tectonic structures and moraine formationQuaternary Science Reviews, 1995
- Consolidation of sediments by glaciers: relations between sediment geotechnics, soft-bed glacier dynamics and subglacial ground-water flowJournal of Glaciology, 1993
- Deep circulation of groundwater in overpressured subglacial aquifers and its geological consequencesQuaternary Science Reviews, 1993
- Anisotropic permeability and tortuosity in deformed wet sedimentsJournal of Geophysical Research, 1990
- Water-Pressure Coupling of Sliding and Bed Deformation: I. Water SystemJournal of Glaciology, 1989
- Shear-zone geometries in experimentally deformed clays: the influence of water content, strain rate and primary fabricJournal of Structural Geology, 1988
- Sediment deformation beneath glaciers: Rheology and geological consequencesJournal of Geophysical Research, 1987
- Clastic dikes formed beneath an active glacierGeologiska Föreningen i Stockholm Förhandlingar, 1986
- The possible mechanics of convolute lamination in graded sand bedsJournal of the Geological Society, 1977
- PERMEABILITY MEASUREMENTS IN THE FIELD AS AN ASSESSMENT OF ANISOTROPY AND STRUCTURE DEVELOPMENTEuropean Journal of Soil Science, 1957