Methodology for searching the displaced part of the coal seam and documentation of disjunctive dislocations for the purpose of classification (From experience of work at the Inta coal deposit)
Authors:
Abstract
Fracture and displacement of the seam is a geological phenomenon that, in each specific case depending on the geological setting, possesses special geometric forms. Geometric classifications of fractures are numerous and their complexity is diverse, but all of them are only a way to make sense of the variety of fracture shapes. In order to search for the displaced part of the seam, data on not only the normal but also the displaced wing are needed. Therefore, geological setting data common to both wings are of particular importance for the search for the displaced part of the seam.
Область исследования:
(Archived) Without section
Funding:
None
References
- Belitsky A. A. Classification of tectonic fractures and geometric methods of their study. Gosgeolizdat, 1953. (in Russian)
- Gzovsky M. V. Basic questions of classification of tectonic ruptures. Sovetskaya geologiya, 1954, No. 41. (in Russian)
- Zabrodin A. S. Experience of searching for the displaced part of the coal seam in disturbed deposits. Ugletekhizdat, 1952. (in Russian)
- Kulikov P. K. Methods of prospecting for the displaced wing of the seam. Ugletekhizdat, 1956. (in Russian)
- Ryzhov P. A. Geometry of the subsurface. Ugletekhizdat, 1952. (in Russian)
- Ushakov I. N. On the simplification of the geometric classification of displacements. Sbornik Issledovaniya po voprosam gornogo i marksheyderskogo dela. Ugletekhizdat, 1957, No. XXXI. (in Russian)
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