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accumulations (grade-thickness) rather than weighted RQD would surely
prove its usefulnessfor geostatistics and for kriging. It is hoped that, in the
future, further trials and prolonged examination will confirm the validity of
a wider application of this technique.
Moreover, an important consequence of stereotomography, along with
ensuing important results, will be the persistence probability. It is believed
that much remains to be investigated by researchers, and that the present
theory which is still at an early stage, will be viable and will lead to more
general development with the help of other geoscientists. Unfortunately,
at the time of our study, the open pit from which the data come, was not
sufficiently advanced for using the available structural geology field data.
Also, it was not possible to confirm retrospectively with a back-analysis
their equivalence with similar data generated by the stereotomographic
technique. Thus, additional tests will be needed for assessing the complete
validity of our method. But the authors remain very optimistic about the
utility of such a technique and they hope that fair competition can stimulate
many interested investigators, and they invite the latter to share their data
and results for the benefit of the whole mining field.
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Barnes, M.P., 1980. Computer-Assisted Mineral Appraisal and Feasibility. AIME,
New York, N.Y., 167 pp.
Brown, E.T., 1981. Rock Characterization Testing and Monitoring - ISRM
Suggested Methods. Pergamon, Oxford, 211 pp.
Davis, J.C., 1973. Statistics and Data Analysis in Geology. Wiley, New York,
N.Y., 550 pp.
Deere, D.U., 1963. Technical description of rock cores for engineering
purposes. Felsmech. Ingenieurgeol. (Rock Mech. Eng. Geol.), 1(1): 16-22.
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