Abstract
"The orientation of crinoid detritus is used to deduce a current pattern in the Carboniferous limestone of the Benbulbin area, County Sligo, in northwest Ireland. Experiments show that orientation of elongated particles by a unidirectional current will be aligned in several maxima. In the investigated environment orientation around the 'b' direction dominates. The frequency diagrams of orientation measurements are best described by harmonic analysis."
This content is PDF only. Please click on the PDF icon to access.
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
