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
dc.subject	brittle-ductile transition
dc.subject	crystalline rocks
dc.subject	fault zones
dc.subject.department	Department of Civil Engineering
dc.title	Crustal permeability	en_US
dc.type	Article	en_US

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