scholarly journals EXPERIMENTAL DETERMINATION OF STRESS PARAMETERS IN THE MINING FIELD

2021 ◽  
Vol 2 (4) ◽  
pp. 123-129
Author(s):  
Alexander A. Skulkin

The experience of measuring the stress state of the rock mass at the Tashtagol iron ore deposit and the result of stresses acting in the induced field in the vicinity of 10 orts at a depth of 800 m from the daily surface (horizon -350) is presented using the method of measuring hydraulic fracturing. Stress concentration zones around the mine are determined at the measuring station.

2019 ◽  
Vol 5 ◽  
pp. 111-123
Author(s):  
V.L. Trushko ◽  
◽  
A.P. Gospodarikov ◽  
K.V. Sozonov ◽  
◽  
...  

2018 ◽  
Vol 54 (1) ◽  
pp. 13-20 ◽  
Author(s):  
G. G. Kocharyan ◽  
S. R. Zolotukhin ◽  
E. V. Kalinin ◽  
L. L. Panas’yan ◽  
V. G. Spungin

Author(s):  
Viktor S. Pisarev ◽  

The relevance of the study is to develop a methodology for monitoring manufacturing objects us-ing unmanned aerial vehicles formed as a result of mining operations. The Tashtagol iron ore deposit is located in the south of the Kemerovo region in Gornaya Shoria, and is being worked underground. The development of the reserves of the South-Eastern section has been carried out since 2004 by the Tashtagol branch of company Evrazruda. A special feature of the South-Eastern section reserves min-ing is the operation of protected objects within the zone of potential hazardous displacements, as a re-sult of which, presumably in November 2017, a sinkhole was formed in the area of Mount Boulanger. The aim of the work is to describe the method of monitoring the determination of the geometric dimensions of the sinkhole in different periods of time using an unmanned aerial vehicle. The sinkhole development has been monitored since 2018. As a result, this study determines the geometric dimensions of the sinkhole in different periods of obser-vations, and calculates the average sinkhole increase dynamics of the per year.


Geophysics ◽  
1955 ◽  
Vol 20 (4) ◽  
pp. 871-885 ◽  
Author(s):  
W. B. Agocs

The airborne magnetometer data of the Marmora iron ore deposit at Marmora, Ontario have been used as an example to show the results obtained by the use of various line spacings ranging from 1 mile to 1/4 mile. The maps show how easy it is, in any type of geophysical survey, to miss a feature of economic value if the line spacing is too coarse. The probability equations are given for the crossing of randomly oriented features whose maximum dimension is less than the spacing of the control lines for circular, elongate, and rectangular outlines. The equations are [Formula: see text]; [Formula: see text]; [Formula: see text]; [Formula: see text]; [Formula: see text]; and [Formula: see text]; respectively where P is the probability; D is the diameter; L is the length; W is the width; and S and T are line spacings.


2019 ◽  
Vol 1 (2) ◽  
pp. 37-41
Author(s):  
Su Kangjie ◽  
Yuan Ya

2019 ◽  
Author(s):  
Bolorchimeg Nanzad ◽  
◽  
Marek Locmelis ◽  
Brandon James Sullivan ◽  
Ryan Mathur

Sign in / Sign up

Export Citation Format

Share Document