Chad Deering
- Associate Professor, Geological and Mining Engineering and Sciences
- Ph.D., Igneous Petrology and Geochemistry, University of Canterbury, New Zealand, Christchurch
Biography
Chad Deering is an Associate Professor in the Department of Geological and Mining Engineering and Sciences at Michigan Technological University. His research focuses on igneous petrology, volcanology, and geochemistry, with an emphasis on understanding the structure, evolution, and dynamics of transcrustal magmatic systems. He integrates field geology, mineral chemistry, thermodynamic modeling, geochronology, and geochemical data analysis to investigate how magmas are generated, stored, and modified through space and time.
A central theme of Dr. Deering’s work is the linkage between magmatic processes, volatile behavior, and the formation of mineral and geothermal resources. His research spans continental arc and rift systems worldwide and has been supported by NSF, NASA, USGS, and international industry partners. He has published extensively in leading journals, including Science, Nature Geoscience, Earth and Planetary Science Letters, and Geology, and currently serves on the editorial board of Minerals.
Dr. Deering is deeply committed to geoscience education and mentoring. He teaches undergraduate and graduate courses in petrology, mineral science, geochemistry, and magma reservoir dynamics, and actively supervises student research that bridges fundamental Earth processes with emerging data-driven and AI-enabled approaches to geoscience problems.
Links of Interest
Specialties
- Source to surface transport of magmatic volatiles and fluid evolution in geothermal systems
- Evolution of the upper continental crust: generation and maintenance of large, silicic magma reservoirs
- Magma reservoir dynamics by quantifying textural fabrics and intracrystalline deformation formed during hindered settling and compaction
- Relationship between resurgent plutons and large, silicic ignimbrites in exhumed caldera-forming eruptive sequences
- Excess or cryptic degassing in volcanic systems
- Quantification of CO2 from diffuse degassing at large, caldera-forming volcanoes