Determination of the Geometric Form of a Plane of a Tectonic Gap as the Inverse III-posed Problem of Mathematical Physics

Sirota, Dmitry; Ivanov, Vadim

doi:10.1051/e3sconf/20172101017

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2018

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“…, where the dimensions of a quantity of w is the meter as in [2,3]. After that the elementary volume dVP is converted to the following dimensionless quantity…”

Section: Let Us Transform the (2) To A Dimensionless Form Bymentioning

confidence: 99%

Diagnostics of the 3D Shape of a Rock Failure Zone by Electrical Measurements on the Earthrs Surface

Sirota¹,

Ivanov²

2018

Proceedings of the 9th China-Russia Symposium “Coal in the 21st Century: Mining, Intelligent Equipment and Environment Protecti

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In a number of previously published papers by D. Sirota and V. Ivanov, it is theoretically and experimentally shown that the electrical measurements on the earth's surface can determine the approximate size and depth of the hearth of a man-made earthquake and a rock bursts in coal seams at depths of the hearth to several hundred meters. To predict the energy of the upcoming seismic event and determine the location of the event, it is necessary to determine the size, shape and orientation of the hearth. Keywordsexploration geophysics, diagnostic problem, interpretation of geophysical data, rock burst, integral equation of the first kind, inverse ill-posed problem, tikhonov regularization method I.

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“…, where the dimensions of a quantity of w is the meter as in [2,3]. After that the elementary volume dVP is converted to the following dimensionless quantity…”

Section: Let Us Transform the (2) To A Dimensionless Form Bymentioning

confidence: 99%