Calculator for designing effective drawpoint bunds.

Understanding the relationship between seismic energy and moment parameters.

Interpreting hazard isosurfaces and spatial distribution of seismic events.

Why event magnitudes differ between software and how to calculate them.

Log scales and Gutenberg-Richter distributions.

The Grid Based Analysis application can be used to evaluate the spatial distribution of various seismic parameters. There are a range of source parameter options available, and they can give indications to the rock mass behaviour. Some parameters can be considered as a proxy (stand-in) for rock mass stress, while other parameters can be a proxy for the amount of deformation. There are also parameters available that are associated with the rock mass mechanism or event type.

Evaluating the spatial distribution of various seismic parameters.

Overview

Event rate calculations and splattering in grid-based hazard assessment.

Estimating seismic hazard for work areas using excavation view analysis.

Mine Geometry Model Minode Generator is a new utility app which enables you to generate your own new minodes from a mine geometry model. If you're not sure what minodes are or why you would want to generate them, see What are minodes? If you're not sure what mine geometry models are, see Mine Geometry Models Application.

IMS and ESG sites should have moment tensors loaded in with the events table automatically.

A geotech's guide to understanding moment tensors.

Tools for monitoring drawpoint conditions and inrush events.

Where is the cumulative energy line on the Omori chart?

Dashboard tools for inrush risk reporting and TARPs.

Physical meaning and calculation methods for seismic energy and moment.

Overview

How b-value sensitivity affects seismic hazard calculations and event rates.

Quick reference guide to seismic source parameters and their meanings.

Quantifying effects of input parameter variations on seismic hazard.

Separating clustered and background seismic events using stochastic methods.

Calculating peak particle velocity from seismic events and ground motion.

That is the question. An explainer on seismic hazard measurement.

New features and advanced tools for hazard assessment analysis.

Framework for monitoring and controlling inrush hazards.

MUL refers to the truncating magnitude of the Gutenberg-Richter distribution