Crustal permeability
| dc.contributor.author | Ingebritsen, Steve | |
| dc.contributor.author | Gleeson, Tom | |
| dc.date.accessioned | 2019-03-02T16:38:38Z | |
| dc.date.available | 2019-03-02T16:38:38Z | |
| dc.date.copyright | 2017 | en_US |
| dc.date.issued | 2017 | |
| dc.description.abstract | Permeability is the dominant parameter in most hydrogeologic studies. There is abundant evidence for dynamic variations in permeability in time as well as space, and throughout the crust. Whether this dynamic behavior should be included in quantitative models depends on the problem at hand. | en_US |
| dc.description.reviewstatus | Reviewed | en_US |
| dc.description.scholarlevel | Faculty | en_US |
| dc.identifier.citation | Ingebritsen, S. & Gleeson, T. (2017). Crustal permeability. Hydrogeology Journal, 25(8), 2221-2224. DOI: 10.1007/s10040-017-1663-4 | en_US |
| dc.identifier.uri | https://doi.org/10.1007/s10040-017-1663-4 | |
| dc.identifier.uri | http://hdl.handle.net/1828/10628 | |
| dc.language.iso | en | en_US |
| dc.publisher | Hydrogeology Journal | en_US |
| dc.subject | permeability | en_US |
| dc.subject | brittle-ductile transition | en_US |
| dc.subject | crystalline rocks | en_US |
| dc.subject | fault zones | en_US |
| dc.title | Crustal permeability | en_US |
| dc.type | Article | en_US |
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