The crustal magmatic structure beneath the Denali Volcanic Gap imaged by a dense linear seismic array
The crustal magmatic structure beneath the Denali Volcanic Gap imaged by a dense linear seismic array
● We present a 2‐D shear velocity model of the top 16 km of the crust in south-central Alaska across the Alaska range.
● The Denali fault was identified as a narrow localized low-velocity anomaly extending to at least 12 km depth.
● We observe a low-velocity zone ~12 km beneath the volcanic gap. We interpret the anomaly as a subduction-related magma reservoir.
Isolating and Tracking Noise Sources across an Active Longwall Mine Using Seismic Interferometry
Isolating and Tracking Noise Sources across an Active Longwall Mine Using Seismic Interferometry
Isolating the mining activity from background noise is important for passive seismic monitoring.
We show that seismic interferometry can be used to identify and track mining activity in a longwall mine.
Our proposed framework can lead to simultaneous monitoring of subsurface seismicity and structure changes.
Seismic imaging for natural resources exploration
Seismic imaging for natural resources exploration
Shale Gas/Oil
Shale Gas/Oil
Master's Thesis
Geothermal
Geothermal
Internship at Zanskar Geothermal & Minerals, Inc.