|
Article |
The stratigraphy of the Bushveld Complex is characterized by laterally continuous horizontal layering. At the interface of some of these layers there are phenomena analogous to flame, load-cast, ball-and-pillow and liquid escape structures of sedimentary rocks. Three plastic deformation styles recognized in the Complex are (i) vertical, (ii) vertical followed by horizontal, and (iii) vertical fluid movement with brittle failure. These post-deposition structures are used to estimate viscosity and density of adjacent layers during consolidation. The distribution of the structures through the mafic sequence provides some information on magma movement and rates of crystal accumulation.
This article has been cited by other articles:
![]() |
P.A.M. Nex Formation of bifurcating chromitite layers of the UG1 in the Bushveld Igneous Complex, an analogy with sand volcanoes Journal of the Geological Society, 2004; 161: 903 - 909. [Abstract] [Full Text] [PDF] |
||||
![]() |
G. Desharnais, D. C. Peck, R.F. J. Scoates, and N. M. Halden THE KO ZONE: A NEW MODEL FOR PGE Cu Ni MINERALIZATION IN THE MARGINAL ZONE OF THE FOX RIVER SILL, NORTHERN MANITOBA, CANADA Can Mineral, 2004; 42: 291 - 302. [Abstract] [Full Text] [PDF] |
||||
![]() |
W.D. Maier, S.-J. Barnes, and M. J. van der Merwe Platinum-group elements in the Pyroxenite Marker, Bushveld Complex: implications for the formation of the Main Zone South African Journal of Geology, 2001; 104: 301 - 308. [Abstract] [Full Text] [PDF] |
||||