Groundwater flow and groundwater-stream interaction in fractured and dipping sedimentary rocks: Insights from numerical models-Reference-Cited by-同舟云学术

Groundwater flow and groundwater-stream interaction in fractured and dipping sedimentary rocks: Insights from numerical models

Published:2007-01 Issue:1 Volume:43 Page:
ISSN:0043-1397
Container-title:Water Resources Research
language:en
Short-container-title:Water Resour. Res.

Author:

Fan Ying¹,Toran Laura²,Schlische Roy W.¹

Affiliation:

1. Department of Geological Sciences; Rutgers-State University of New Jersey; Piscataway New Jersey USA

2. Department of Geology; Temple University; Philadelphia Pennsylvania USA

Publisher

American Geophysical Union (AGU)

Subject

Water Science and Technology

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1029/2006WR004864/fullpdf

Reference32 articles.

1. Ackermann , R. V. 1997 Spatial distribution of rift-related fractures: Field observations, experimental modeling, and influence on drainage networks Dep. of Geol. Sci., Rutgers-State Univ. of N. J. New Brunswick

2. Influence of fracture anisotropy on groundwater ages and chemistry, Valley and Ridge Province, Pennsylvania;Burton;Ground Water,2002

3. Carleton , G. B. C. Welty H. T. Buxton 1999 Design and analysis of tracer tests to determine effective porosity and dispersivity in fractured sedimentary rocks, Newark Basin, New Jersey U.S. Geol. Surv. Water Resour. Invest. Rep., 98-4126

4. Delineating and quantifying ground water discharge zones using streambed temperatures;Conant;Ground Water,2004

5. Origin of fibrous gypsum in the Newark rift basin, eastern North America;El Tabakh;J. Sediment. Res.,1998

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