Abstract
The monitoring of microseismic activity in geological formations of underground mines is discussed. The accuracy of a particular monitoring technique is subject to limitations of measurement precision, and errors in the determination of the correct phase of the incoming signal associated with the first arrival of the seismic wave. The value of the simplex technique for microseismic monitoring is illustrated through the presentation of experimental results in the determination of source location for a series of known-source test blasts. It is concluded that a careful analysis of the errors affecting each particular microseismic installation is a necessary step in understanding the capabilities of this particular system.< <ETX xmlns:mml="http://www.w3.org/1998/Math/MathML" xmlns:xlink="http://www.w3.org/1999/xlink">></ETX>
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
