Is in situ stress important to groundwater flow in shallow fractured rock aquifers?-Reference-Cited by-同舟云学术

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Is in situ stress important to groundwater flow in shallow fractured rock aquifers?

Published:2011-03 Issue:3-4 Volume:399 Page:185-200
ISSN:0022-1694
Container-title:Journal of Hydrology
language:en
Short-container-title:Journal of Hydrology

Author:

Mortimer L.,Aydin A.,Simmons C.T.,Love A.J.

Publisher

Elsevier BV

Subject

Water Science and Technology

Reference47 articles.

1. The Dynamics of Faulting and Dyke Formation with Application to Britain;Anderson,1951

2. Engineering properties and characterization of rock discontinuities;Bandis,1993

3. Permeability and stress in crystalline rocks;Banks;Terra Review,1996

4. Strength, deformation and conductivity coupling of rock joints;Barton;International Journal of Rock Mechanics and Mining Sciences and Geomechanics Abstracts,1985

5. The shear strength of rock joints in theory and practice;Barton;Rock Mechanics,1977

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1. Bedrock Fractures Control Groundwater‐Driven Mountain Slope Deformations;Journal of Geophysical Research: Earth Surface;2023-11

2. Influence of geological discontinuities on the groundwater flow of the Serra Geral Fractured Aquifer System;Groundwater for Sustainable Development;2022-08

3. Major and trace element hydrogeochemistry of fractured igneous aquifers located in an active strike-slip fault zone: example of the Gezin district (Elazığ, Turkey) in the Eastern Anatolian Fault Zone;Arabian Journal of Geosciences;2022-05

4. Improving local mean stress estimation using Bayesian hierarchical modelling;International Journal of Rock Mechanics and Mining Sciences;2021-12

5. Analysis of the distribution characteristics and laws of in situ stress in China’s coal mines;Arabian Journal of Geosciences;2020-06

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