Microstructures grown experimentally from advectivesupersaturated solution and their implication for natural vein systems

[1]  P. Bons,et al.  Development of crystal morphology during unitaxial growth in a progressively widening vein : II. Numerical simulations of the evolution of antitaxial fibrous veins , 2001 .

[2]  P. Bons,et al.  Mechanisms of fluid flow and fluid–rock interaction in fossil metamorphic hydrothermal systems inferred from vein–wallrock patterns, geometry and microstructure , 2001 .

[3]  C. Passchier,et al.  Numerical simulation of fibre growth in antitaxial strain fringes , 2000 .

[4]  R. Worden Fluid Flow and Transport in Rocks: Mechanisms and Effects , 1998 .

[5]  S. Roberts,et al.  Transient Versus Continuous Fluid Flow in Seismically Active Faults: An Investigation by Electric Analogue and Numerical Modelling , 1997 .

[6]  C. Heinrich,et al.  Chemical mass transfer modelling of ore-forming hydrothermal systems: current practise and problems , 1996 .

[7]  B. Jamtveit,et al.  FLUID FLOW AND TRANSPORT IN ROCKS , 1996 .

[8]  C. Steefel,et al.  A coupled model for transport of multiple chemical species and kinetic precipitation/dissolution rea , 1994 .

[9]  Susan L. Brantley,et al.  Models of quartz overgrowth and vein formation: Deformation and episodic fluid flow in an ancient subduction zone , 1992 .

[10]  S. Cox,et al.  Crack-seal fibre growth mechanisms and their significance in the development of oriented layer silicate microstructures , 1983 .

[11]  John G. Ramsay,et al.  The crack–seal mechanism of rock deformation , 1980, Nature.

[12]  R. Scholten,et al.  Gravity and tectonics , 1973 .

[13]  S. Bajaj Kinetics of crystallization from solutions and melts , 1969 .

[14]  I. Sunagawa Growth History of Crystals in Nature , 1968 .

[15]  C. Hulin Structural control of ore deposition , 1929 .