Table of Contents
Textures and Microstructures
Volume 25, Issue 2-4, Pages 245-250

Joints Orientation Distributions in Sedimentary Rocks

T. P. Belousov,1,2 Sh. A. Mukhamediev,1,2 and S. F. Kurtasov1,2

1Institute of Physics of the Earth, B. Gruzinskaya str., 10, Moscow 123810, Russia
2Institute of Geosystems, Varshavskoye h., 8, Moscow 113105, Russia

Received 30 June 1995

Copyright © 1996 Hindawi Publishing Corporation. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


The results of several years (1980–1994) field observations of rock joints at the former USSR territory are integrated. New methods of data processing and interpretation are proposed and developed. With the local data set for an exposure we connect the symmetric positively defined second order tensor J characterizing the density and relative position of joint systems as well as their orientation in space. The complete set of tensors J for any region depicted in appropriate manner gives the integral “portrait” of tectonic fracturing of the region. The regular changes of such integral characteristics for Great Caucasus as an example are determined.