Analysis of subsurface flow and formation anisotropy in a fractured aquitard using transient water level data-Reference-Cited by-同舟云学术

Analysis of subsurface flow and formation anisotropy in a fractured aquitard using transient water level data

Published:1992-01 Issue:1 Volume:28 Page:199-207
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Rophe B.,Berkowitz B.,Magaritz M.,Ronen D.

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/91WR02181/fullpdf

Reference32 articles.

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2. Bahat , D. Two styles of jointing in chalks and bimodality of joint length distribution revealed by the investigation of plumes on fracture surfaces 1986

3. Joints and en echelon cracks in Middle Eocene chalks near Bear Sheva, Israel;Bahat;J. Struct. Geol.,1986

4. Bahat , D. A tectonic model of the Bear Sheva Eocene chalks 1987

5. Correlation between fracture surface morphology and orientation of cross-fold joints in Eocene chalks around Bear Sheva, Israel;Bahat;Tectonophysics,1987

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5. Eight distinct fault-joint geometric/genetic relationships in the Beer Sheva syncline, Israel;Geological Society, London, Special Publications;2004