UNIVERSAL TEST SYSTEM USED FOR MOLECULAR BIOLOGICAL ANALYSIS OF MICROBIAL COMMUNITIES OF SULFIDE ORE DEPOSITS

2017 ◽  
Vol 12 (32) ◽  
pp. 295-302
Author(s):  
S.V. Rogatykh ◽  
Elements ◽  
2017 ◽  
Vol 13 (2) ◽  
pp. 89-95 ◽  
Author(s):  
Stephen J. Barnes ◽  
David A. Holwell ◽  
Margaux Le Vaillant

2020 ◽  
Vol 192 ◽  
pp. 03005
Author(s):  
Gennady Einbinder ◽  
Natalia Mitishova ◽  
Dmitry Radchenko ◽  
Egor Knyazkin

In the modern conditions, the scale of subsoil transformation in the process of mineral extraction is characterized by an increased risk of accidents, often accompanied by man-made disasters. In this regard, hazard analysis and accident risk assessment is the most important scientific and technical task, the solution of which is based on methods for identification of hazards, study of development trends and assessment of consequences of theoretically possible accidents. In relation to development conditions of sulfide ore deposits, only an accident risk assessment with determination of the possible accident hazard degree, as well as preparation and timely correction of measures aimed at reduction of accident risks can ensure an acceptable level of industrial safety at the hazardous production facility.


Geophysics ◽  
2012 ◽  
Vol 77 (5) ◽  
pp. WC3-WC13 ◽  
Author(s):  
Christof Mueller ◽  
Gilles Bellefleur ◽  
Erick Adam ◽  
Gervais Perron ◽  
Marko Mah ◽  
...  

The Downhole Seismic Imaging consortium conducted two consecutive vertical seismic profiling surveys in the Norman West mining camp (Sudbury, Canada) in 1998 and 1999. These were aimed toward imaging a massive sulfide ore deposit situated within the footwall of the Sudbury Igneous Complex (SIC). Three-component seismic data were acquired in four boreholes with variable signal-to-noise ratio and poor polarization quality. Consequently, the images suffered from strong azimuthal ambiguity. A strike filter, passing only reflections originating from within the SIC, was applied during migration to enhance interpretability of the images obtained. Migrated images showed structures correlating with the known position of an ore deposit located 1800 m away from one borehole (N40). Diffraction coherency migration enhanced the image of the deposit, and suggested strong seismic scattering from within the footwall of the SIC.


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