Characterization of the structure and permeability of shear zones in a siliciclastic aquifer /
This research has shown that the hydraulic conductance of a fault, a quantitative measure of the flow attributes of a fault, is a function of shear-zone permeability, thickness, mudstone fraction and stratigraphic throw. This was accomplished through the characterization of the structure and permea...
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| Format: | Thesis Book |
| Language: | English |
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[Place of publication not identified] :
[publisher not identified] ;
2000.
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| Online Access: | http://proxy.library.tamu.edu/login?url=http://proquest.umi.com/pqdweb?did=731980811&sid=1&Fmt=2&clientId=2945&RQT=309&VName=PQD |
Internet
http://proxy.library.tamu.edu/login?url=http://proquest.umi.com/pqdweb?did=731980811&sid=1&Fmt=2&clientId=2945&RQT=309&VName=PQDCushing: Theses & Dissertations Microforms (Does not check out)
| Call Number: |
2000 Dissertation I33 |
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| Call Number | Status | Get It |
| 2000 Dissertation I33 | Available | |
Available Online
| Call Number: |
2000 Dissertation I33 |
|
|---|---|---|
| Call Number | Status | Get It |
| 2000 Dissertation I33 | Available | |