An experiment with pure gypsum powder to test the applicability of this powder for the formation of open fractures. The inclusion of sand layers in cohesive Hemihydrate (CaSO4 • ½ H2O) powder leads to much wider and complex deformation zones (compare with http://www.youtube.com/watch?v=MmgYBsHuVHk). The sand layers smear into structures similar to clay smears (compare with http://www.youtube.com/watch?v=bhWwdPJbDTQ) in these zones.
This movie is taken from the MSC-thesis of Heijn van Gent. See for more information: van Gent, H. W., Holland, M., Urai, J. L. & Loosveld, R. 2010. Evolution of fault zones in carbonates with mechanical stratigraphy - insights from scale models using layered cohesive powder. Journal of Structural Geology - Special publication: Faulting and fracturing of carbonate rocks: New insights into deformation mechanisms, petrophysics and fluid flow properties 32 (9), 1375-1391. http://dx.doi.org/10.1016/j.jsg.2009.05.006
Yes, we tried to model structures like the East African Rift, or faults in carbonates.
StrucGeology 1 year ago