WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION

Production processes in underground mining provoke stress changes, rock failure, and seismicity. Large seismic event followed by its aftershocks causes damage to production area. Re-entry protocol restricts access to the affected areas during this time of elevated seismic activity in order to distan...

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Main Author: Amalia, Rizka
Format: Theses
Language:Indonesia
Online Access:https://digilib.itb.ac.id/gdl/view/61773
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Institution: Institut Teknologi Bandung
Language: Indonesia
id id-itb.:61773
spelling id-itb.:617732021-09-27T19:34:18ZWAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION Amalia, Rizka Indonesia Theses aftershock, microseismic, Omori’s Law, re-entry protocol, waveform cross correlation INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/61773 Production processes in underground mining provoke stress changes, rock failure, and seismicity. Large seismic event followed by its aftershocks causes damage to production area. Re-entry protocol restricts access to the affected areas during this time of elevated seismic activity in order to distance mine workers from the disaster. In this research, the author evaluates the decay rate of seismicity whereby the aftershocks are sequenced by waveform similarity. Cross correlation is applied to the recorded waveform following large seismic event. Secondly, curve fitting is assigned to the decay rate, and re-entry time is determined afterwards. Aftershock sequences are investigated from 20 distinct significant events resulting in 2 classes in which each feature differs. The result shows that the cross-correlation method is robustly able to detect aftershock sequence by ???????????????? 1.956 30th October 2019 event, located around the source up to 500 meters apart with the re-entry time of 19.145 hours where it is interpreted as shearing on the lithological contact and so the seismicity propagated anisotropically to the cave front which has acted as a weak zone. On the other hand, the second class depicts ???????????????? 2.2 11th April 2019 event yielding the re-entry time of 0.801 hours as well as detecting its aftershock sequence with the distance ranging from 400-1000 meters apart. This pattern of seismicity which has shown the existence of seismic gap is interpreted as crack opening mechanism resulted by stress migration from the cave to weak zone inducing seismic cluster 600 meters apart from the major event. text
institution Institut Teknologi Bandung
building Institut Teknologi Bandung Library
continent Asia
country Indonesia
Indonesia
content_provider Institut Teknologi Bandung
collection Digital ITB
language Indonesia
description Production processes in underground mining provoke stress changes, rock failure, and seismicity. Large seismic event followed by its aftershocks causes damage to production area. Re-entry protocol restricts access to the affected areas during this time of elevated seismic activity in order to distance mine workers from the disaster. In this research, the author evaluates the decay rate of seismicity whereby the aftershocks are sequenced by waveform similarity. Cross correlation is applied to the recorded waveform following large seismic event. Secondly, curve fitting is assigned to the decay rate, and re-entry time is determined afterwards. Aftershock sequences are investigated from 20 distinct significant events resulting in 2 classes in which each feature differs. The result shows that the cross-correlation method is robustly able to detect aftershock sequence by ???????????????? 1.956 30th October 2019 event, located around the source up to 500 meters apart with the re-entry time of 19.145 hours where it is interpreted as shearing on the lithological contact and so the seismicity propagated anisotropically to the cave front which has acted as a weak zone. On the other hand, the second class depicts ???????????????? 2.2 11th April 2019 event yielding the re-entry time of 0.801 hours as well as detecting its aftershock sequence with the distance ranging from 400-1000 meters apart. This pattern of seismicity which has shown the existence of seismic gap is interpreted as crack opening mechanism resulted by stress migration from the cave to weak zone inducing seismic cluster 600 meters apart from the major event.
format Theses
author Amalia, Rizka
spellingShingle Amalia, Rizka
WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
author_facet Amalia, Rizka
author_sort Amalia, Rizka
title WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
title_short WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
title_full WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
title_fullStr WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
title_full_unstemmed WAVEFORM CROSS CORRELATION ANALYSIS FOR AFTERSHOCK DECAY MONITORING IN MINING REGION
title_sort waveform cross correlation analysis for aftershock decay monitoring in mining region
url https://digilib.itb.ac.id/gdl/view/61773
_version_ 1822003926624370688