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Identification of rock mass discontinuities in a cluster of seismic event hypocenters.

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dc.contributor.author Kijko, A
dc.contributor.author Lasocki, S
dc.contributor.author Retief, SJP
dc.date.accessioned 2007-12-14T07:41:40Z
dc.date.available 2007-12-14T07:41:40Z
dc.date.issued 1999
dc.identifier.citation Kijko, A, Lasocki, S and Retief, SJP. 1999. Identification of rock mass discontinuities in a cluster of seismic event hypocenters. Safety in Mines Research Advisory Committee, GAP 622, 1999, pp 1-20 en
dc.identifier.uri http://hdl.handle.net/10204/1795
dc.description.abstract A technique to interpret a cluster of seismic events in terms of causative structures is described. The process consists of moving the located hypocenters of events within their confidence ellipsoids until a simplified pattern of the seismic event cluster is obtained. This simplified pattern might then be interpreted in terms of a fault, a system of faults or in general, as a rock mass discontinuity. The process is tested and demonstrated for three synthetic sets of data: a single fault, two joined faults and three separate faults. en
dc.language.iso en en
dc.subject SIMRAC en
dc.subject GAP 622 en
dc.subject Rock mass discontinuities en
dc.subject Seismic events en
dc.title Identification of rock mass discontinuities in a cluster of seismic event hypocenters. en
dc.type Conference Presentation en
dc.identifier.apacitation Kijko, A., Lasocki, S., & Retief, S. (1999). Identification of rock mass discontinuities in a cluster of seismic event hypocenters. http://hdl.handle.net/10204/1795 en_ZA
dc.identifier.chicagocitation Kijko, A, S Lasocki, and SJP Retief. "Identification of rock mass discontinuities in a cluster of seismic event hypocenters." (1999): http://hdl.handle.net/10204/1795 en_ZA
dc.identifier.vancouvercitation Kijko A, Lasocki S, Retief S, Identification of rock mass discontinuities in a cluster of seismic event hypocenters; 1999. http://hdl.handle.net/10204/1795 . en_ZA
dc.identifier.ris TY - Conference Presentation AU - Kijko, A AU - Lasocki, S AU - Retief, SJP AB - A technique to interpret a cluster of seismic events in terms of causative structures is described. The process consists of moving the located hypocenters of events within their confidence ellipsoids until a simplified pattern of the seismic event cluster is obtained. This simplified pattern might then be interpreted in terms of a fault, a system of faults or in general, as a rock mass discontinuity. The process is tested and demonstrated for three synthetic sets of data: a single fault, two joined faults and three separate faults. DA - 1999 DB - ResearchSpace DP - CSIR KW - SIMRAC KW - GAP 622 KW - Rock mass discontinuities KW - Seismic events LK - https://researchspace.csir.co.za PY - 1999 T1 - Identification of rock mass discontinuities in a cluster of seismic event hypocenters TI - Identification of rock mass discontinuities in a cluster of seismic event hypocenters UR - http://hdl.handle.net/10204/1795 ER - en_ZA


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