2002
Król, M.; Tomaszewska, R.
Comparison of direct structural research and shallow seismic refraction method in systematic joints study Journal Article
In: Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea, vol. 24, no. 340, pp. 413-418, 2002, ISSN: 0138015X.
@article{2-s2.0-0036997658,
title = {Comparison of direct structural research and shallow seismic refraction method in systematic joints study},
author = { M. Król and R. Tomaszewska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0036997658&partnerID=40&md5=eb19b62bb4c6d0b453a9251057b6ff77},
issn = {0138015X},
year = {2002},
date = {2002-01-01},
journal = {Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea},
volume = {24},
number = {340},
pages = {413-418},
abstract = {The paper presents results of measurements of seismic wave velocity anisotropy. The results obtained were compared with direct structural measurements. The investigations were carried out in the Triassic carbonate deposits in the NE margin of the Upper Silesian Coal Basin (the USCB). Three areas have been chosen: Strzyzowice, Ujejsce, Strzemieszyce. The velocity of wave propagation was measured in profiles which were radially set, so it was possible to determine the orientation of fracture in the rock mass. The results were estimated on the basis of 2-rank and 4-rank tensors. In the case of strong anisotropy of seismic waves and small numbers of joint sets, there was a good correlation of seismic and structural measurements.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
The paper presents results of measurements of seismic wave velocity anisotropy. The results obtained were compared with direct structural measurements. The investigations were carried out in the Triassic carbonate deposits in the NE margin of the Upper Silesian Coal Basin (the USCB). Three areas have been chosen: Strzyzowice, Ujejsce, Strzemieszyce. The velocity of wave propagation was measured in profiles which were radially set, so it was possible to determine the orientation of fracture in the rock mass. The results were estimated on the basis of 2-rank and 4-rank tensors. In the case of strong anisotropy of seismic waves and small numbers of joint sets, there was a good correlation of seismic and structural measurements.