1887

Abstract

The anisotropy of shales results from a partial alignment of anisotropic plate-like clay minerals. Slow sedimentation of clay minerals from dilute suspension favours face-to-face aggregation to foren `domains' of parallel clay platelets as shown in figure 1.

Loading

Article metrics loading...

/content/papers/10.3997/2214-4609.201409202
1995-05-29
2020-09-19
Loading full text...

Full text loading...

http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409202
Loading
This is a required field
Please enter a valid email address
Approval was a Success
Invalid data
An Error Occurred
Approval was partially successful, following selected items could not be processed due to error