The fracture permeability of Hard Rock Aquifers is due neither to tectonics, nor to unloading, but to weathering processes

Patrick Lachassagne, Robert Wyns, Benoît Dewandel

Open source

DOI: 10.1111/j.1365-3121.2011.00998.x
Published: 2011-04-25
Container: Terra Nova
Publisher: Wiley
Open access: unknown

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Cite this work

BibTeX

@article{allodium:10.1111/j.1365-3121.2011.00998.x,
  title = {The fracture permeability of Hard Rock Aquifers is due neither to tectonics, nor to unloading, but to weathering processes},
  author = {Patrick Lachassagne and Robert Wyns and Benoît Dewandel},
  year = {2011},
  journal = {Terra Nova},
  doi = {10.1111/j.1365-3121.2011.00998.x},
  url = {https://doi.org/10.1111/j.1365-3121.2011.00998.x}
}

RIS

TY  - JOUR
TI  - The fracture permeability of Hard Rock Aquifers is due neither to tectonics, nor to unloading, but to weathering processes
AU  - Patrick Lachassagne
AU  - Robert Wyns
AU  - Benoît Dewandel
PY  - 2011
JO  - Terra Nova
DO  - 10.1111/j.1365-3121.2011.00998.x
UR  - https://doi.org/10.1111/j.1365-3121.2011.00998.x
ER  -

APA

Lachassagne, P., Wyns, R., & Dewandel, B. (2011). The fracture permeability of Hard Rock Aquifers is due neither to tectonics, nor to unloading, but to weathering processes. Terra Nova. https://doi.org/10.1111/j.1365-3121.2011.00998.x

Source records

crossref · retrieved 2026-09-26T01:21:08.351Z