11 research outputs found
Optimum use of water for industry and agriculture Phase 3
Includes bibliographical referencesAvailable from British Library Document Supply Centre- DSC:m03/20514 / BLDSC - British Library Document Supply CentreSIGLEGBUnited Kingdo
Optimum use of water for industry and agriculture Phase 3 : best practice manual
SIGLEAvailable from British Library Document Supply Centre- DSC:7218. 47445(056/TR2) / BLDSC - British Library Document Supply CentreGBUnited Kingdo
Investigate the possible reduction of mine water ingress by introducing tree plantations: Case study of Cooke 4 mine (South Africa)
“The child can remember your voice”: parent–child communication about sexuality in the South African context
Evaluating available solar photovoltaic business opportunities in coal phase-out regions – An energy transition case of Steve Tshwete local municipality in South Africa
How participatory mapping can drive community empowerment – a case study of Koffiekraal, South Africa
Factors affecting fluid flow in strike–slip fault systems:\ud coupled deformation and fluid flow modelling with\ud application to the western Mount Isa Inlier, Australia
Deformation and focused fluid flow within a mineralized system are critical in the genesis of hydrothermal ore\ud
deposits. Dilation and integrated fluid flux due to coupled deformation and fluid flow in simple strike–slip fault\ud
geometries were examined using finite difference analysis in three dimensions. A series of generic fault bend and\ud
fault jog geometries consistent with those seen in the western Mount Isa Inlier were modelled in order to understand how fault geometry parameters influence the dilation and integrated fluid flux. Fault dip, fault width,\ud
bend ⁄ jog angle, and length were varied, and a cross-cutting fault and contrasting rock types were included. The\ud
results demonstrate that low fault dips, the presence of contrasts in rock type, and wide faults produce highest\ud
dilation and integrated fluid flux values. Increasing fault bend lengths and angles increases dilation and integrated\ud
fluid flux, but increasing fault jog length or angle has the opposite effect. There is minimal difference between\ud
the outputs from the releasing and restraining fault bend and jog geometries. Model characteristics producing\ud
greater fluid flows and ⁄ or gradients can be used in a predictive capacity in order to focus exploration on regions\ud
with more favorable fault geometries, provided that the mineralized rocks had Mohr–Coulomb rheologies similar\ud
to the ones used in the models
