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Updated: May 22, 2026

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Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
Published on: August 7, 2017
Linking petrology and seismology at an active volcano
Kate Saunders1, Jon Blundy, Ralf Dohmen
1Department of Earth Sciences, University of Bristol, Bristol, UK. Kate.Saunders@bristol.ac.uk
Summary
Volcanic unrest signals, like seismicity, can indicate magma movement. Studying orthopyroxene crystals from Mount St. Helens reveals magma intrusions correlate with seismic events, improving eruption forecasting.
Area of Science:
- * Volcanology
- * Petrology
- * Geophysics
Background:
- * Active volcanoes show pre-eruptive changes in seismicity, ground deformation, and gas emissions.
- * Interpreting these unrest signals in terms of subsurface magmatic processes remains a significant challenge in volcano monitoring.
- * Understanding magma movement is crucial for predicting volcanic eruptions.
Purpose of the Study:
- * To investigate the relationship between magma intrusions and seismicity preceding volcanic eruptions.
- * To utilize petrological data from volcanic crystals to understand subterranean magmatic processes.
- * To enhance the accuracy of volcanic eruption forecasting through detailed analysis of eruptive products.
Main Methods:
- * Analysis of over 300 zoned orthopyroxene crystals from the 1980-1986 Mount St. Helens eruption.
- * Application of diffusion chronometry to orthopyroxene crystal rims to determine timing of events.
- * Correlation of petrological data with historical seismicity records.
Main Results:
- * Orthopyroxene crystals recorded pulsatory intrusions of new magma and volatiles into a larger magma reservoir.
- * Diffusion chronometry indicated temporal correlation between magma intrusion episodes and recorded seismicity.
- * Evidence suggests that some seismic events are directly linked to magma intrusion processes.
Conclusions:
- * Petrological analysis of crystals provides insights into the timing and nature of pre-eruptive magmatic activity.
- * The timescales of magma intrusion events align with monitoring signals observed at restless volcanoes.
- * This study improves the ability to forecast volcanic eruptions by linking petrologic observations to seismic monitoring data.
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