TY  - BOOK
AU  - Zhang,X.
AU  - Sanderson,D.J.
TI  - Numerical modelling and analysis of fluid flow and deformation of fractured rock masses
SN  - 9780080537863
AV  - TA706 .Z45 2002eb
U1  - 624.1/5132 22
PY  - 2002///
CY  - Amsterdam, Boston
PB  - Pergamon
KW  - Rocks
KW  - Fracture
KW  - Mathematical models
KW  - Rock mechanics
KW  - Fluid dynamics
KW  - Rock deformation
KW  - Roches
KW  - Fracturation
KW  - Modèles mathématiques
KW  - Déformation
KW  - Dynamique des fluides
KW  - Mécanique des roches
KW  - TECHNOLOGY & ENGINEERING
KW  - Civil
KW  - Soil & Rock
KW  - bisacsh
KW  - fast
KW  - Electronic books
N1  - Includes bibliographical references (pages 261-275) and index; Front Cover; Numerical Modelling and Analysis of Fluid Flow and Deformation of Fractured Rock Masses; Copyright Page; Preface; Contents; Chapter 1. Introduction to Modelling Deformation and Fluid Flow of Fractured Rock; Chapter 2. Modelling of Simple Rock Blocks; Chapter 3. Evaluation of 2-Dimensional Permeability Tensors; Chapter 4. Scaling of 2-D Permeability Tensors; Chapter 5. Percolation Behaviour of Fracture Networks; Chapter 6. Slip and Fluid Flow around An Extensional Fault; Chapter 7. Instability and Associated Localization of Deformation and Fluid Flow in Fractured Rocks; Electronic reproduction; [Place of publication not identified]; HathiTrust Digital Library; 2010
N2  - Our understanding of the subsurface system of the earth is becoming increasingly more sophisticated both at the level of the behaviour of its components (solid, liquid and gas) as well as their variations in space and time. The implementation of coupled models is essential for the understanding of an increasing number of natural phenomena and in predicting human impact on these. The growing interest in the relation between fluid flow and deformation in subsurface rock systems that characterise the upper crust has led to increasingly specialized knowledge in many branches of earth sciences and
UR  - https://search.ebscohost.com/login.aspx?direct=true&scope=site&db=nlebk&AN=210029
ER  -