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Record W7162078145 · doi:10.82308/33300

Effect of mining and geology on induced seismicity - A case study

2023· dissertation· en· W7162078145 on OpenAlexaboutno aff
Heba Khalil

Bibliographic record

Venuenot available
Typedissertation
Languageen
FieldEarth and Planetary Sciences
TopicSeismic Imaging and Inversion Techniques
Canadian institutionsnot available
Fundersnot available
KeywordsInduced seismicityMicroseismStopingMagnitude (astronomy)Gold miningFracture (geology)Range (aeronautics)Underground mining (soft rock)

Abstract

fetched live from OpenAlex

High in-situ stresses are expected to induce stronger micro-seismicity as mining production advances to deeper levels. Strong seismic events could cause rockmass and support system damage in drifts and stopes resulting in production delays. Mining-induced seismicity is influenced by a wide range of mining and geology parameters, most notably, stope dimensions, mining sequence, production rate, and geological structures in the vicinity of the work areas. Analyzing the root causes of strong seismic activities can help better understand the influences of such parameters. It could also prove useful for mine planning to mitigate the occurrence of strong seismic events and to provide a safer work environment. This thesis reports the results of a case study of Young-Davidson (YD) mine of Alamos Gold Inc. in northern Ontario, a gold mining operation using sublevel stoping method. The goal of the research is to conduct a comprehensive study of the microseismic database to discern the root causes of large micro-seismic events. Seismic events of magnitude Mn 2.0+ have been observed at mining depths of only 600 m to 800 m below surface, while strong seismic activities are normally expected to be associated with deep excavations. The occurrence of such large events at shallow depth is the key issue of the first part of the study. Statistical methods are utilized to analyze seismic data and relate it to mining activity. Variation in b-value, derived from the microseismic event magnitude-frequency distribution, is used to identify the rock unstable zones. It is used to differentiate between high and low stress zones and to examine the effect of geological structures, specifically the diabase dykes in the mining area. Furthermore, moment tensor inversion is carried out with MATLAB to analyze micro-seismicity, discern the mechanisms of rock failure. In the second part of the study, analysis of seismic events of magnitude Mn 2.0+, that were observed in the lower-mine zone, is conducted. Moment tensor inversion of these large events is carried out to identify the rock failure mechanisms using ESG HSS-Advanced seismic analysis software. In-situ stress measurements previously conducted at the YD mine are analyzed and used to generate a 3D numerical model with finite difference software FLAC3D taking into consideration the intersecting dykes. Mine-wide modelling aims to simulate mining-induced stress distribution per the mine plan of primary and secondary stope extraction sequence. Assessment of stress distribution, brittle shear ratio, and strain energy, as well as comparison with seismic source location, magnitude, and mechanism are discussed. Although the findings from this study are specific to the YD mine, they can also be used to elucidate the causes of seismicity in other mines with similar conditions

Fetched live from OpenAlex and de-inverted. Abstracts are not stored in this database: the inverted indexes are 8.6 GB of the frame’s 9.3 GB of text, and the host has 13 GB free.

How this classification was reachedexpand

Full frame machine prediction

Teacher imitation

Not calibrated prevalence, not ground truth. Human validation pending. The Gemma side is a direct model label for every work in the frame, read from the title-only record. The Codex side is a classifier learned from the 10,348 direct Codex labels and calibrated to design-weighted sample rates; fields without enough sample support carry no Codex call. Candidate is the union of the two sides; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels.

metaresearch head score (Codex)0.000
metaresearch head score (Gemma)0.001
Version: metacan-v3-hybrid-931329e0061cValidation status: machine_predicted_unvalidated
Candidate categoriesnone
Consensus categoriesnone
DomainCandidate signal: none · Consensus signal: none
Study designCandidate signal: Observational · Consensus signal: Observational
GenreCandidate signal: Empirical · Consensus signal: Empirical
Teacher disagreement score0.033
Threshold uncertainty score0.066

Distilled classifier scores by category (both heads)

CategoryCodexGemma
Metaresearch0.0000.001
Meta-epidemiology (narrow)0.0000.000
Meta-epidemiology (broad)0.0000.000
Bibliometrics0.0010.002
Science and technology studies0.0010.000
Scholarly communication0.0010.000
Open science0.0010.000
Research integrity0.0010.000
Insufficient payload (model declined to judge)0.0010.000

Machine scores (provisional)

The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.

Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.

Opus teacher head0.019
GPT teacher head0.285
Teacher spread0.265 · how far apart the two teachers sit on this one work
Validation statusscore_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from it

Classification

machine, unvalidated

Machine predicted; a candidate call from one source (direct Gemma or distilled Codex), not a consensus.

The models applied no category: nothing in the taxonomy fit this work.
Study designObservational
Domainnot available
GenreEmpirical

How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".

Quick stats

Citations0
Published2023
Admission routes1
Has abstractyes

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