Mario A. Guzman, Ph.D.
Mario Guzman is an Economic Geologist with the Geology, Geophysics, and Geochemistry Science Center.
Mario specializes in the formation of base and precious metal ores, with a primary focus on porphyry and epithermal mineral deposits. His investigations utilize field observations, mineral and fluid inclusion petrography, microanalytical techniques, and geochronology. Through these approaches, he uncovers critical insights into the conditions of metal enrichment, fluid evolution, and mineralization mechanisms.
His expertise extends from studying epithermal vein deposits in the San Juan Volcanic Field in Southwest Colorado to porphyry copper deposits and Climax-type porphyry molybdenum deposits. Mario delves into the precipitation mechanisms of hydrothermal fluids at ore deposits and both liquid-dominated and vapor-dominated geothermal systems.
Mario's doctoral research centered on fluid flashing and mineral precipitation within intermediate sulfidation epithermal vein deposits at the Creede and Sunnyside deposits in Southwest Colorado. During his graduate studies, he enriched his understanding as a visiting research geoscientist at Kyushu University, studying the formation of low- and high-sulfidation epithermal deposits, as well as mineral scaling in liquid-dominated geothermal fields.
His research experience further includes investigations into mineral scaling from The Geysers vapor-dominated geothermal field in California and the analysis of fumaroles from volcanoes in Ecuador. Before joining GGGSC in Denver, Mario was a Physical Science Lab Technician at the USGS Water Resources Mission Area in Boulder, Colorado where he conducted essential x-ray diffraction and wavelength dispersive x-ray fluorescence analyses for various research projects.
Professional Experience
Advisory Board Member, Department of Geological Sciences, University of Colorado at Boulder (2024-present)
Pathways Career Intern (Geology), U.S. Geological Survey (2016-2024)
Exploration Geologist, Hecla Mining Company (2012-2013)
Physical Science Lab Technician, U.S. Geological Survey (2009-2012)
Education and Certifications
Ph.D., Geological Sciences, Colorado School of Mines, 2024
M.S., Geological Sciences, Colorado School of Mines, 2016
B.A., Geological Sciences, University of Colorado, Boulder, 2012
B.A., Anthropology, University of Colorado, Boulder, 2008
Affiliations and Memberships*
Society of Economic Geologists
Geological Society of America
Denver Region Exploration Geologists Society
Geochemical Society
Commission on the Chemistry of Volcanic Gases
Rocky Mountain Association of Geologists
Colorado Scientific Society
Science and Products
Evidence for a high-level porphyritic intrusion below the Sunnyside epithermal vein deposit, Colorado
High-temperature quartz veins were identified in drill core at ~600 m below the Sunnyside epithermal base and pre-cious metal deposit in southwestern Colorado. The veins consist of early anhedral quartz that shows a bluish ca-thodoluminescence emission and hosts heterogenous silicate melt inclusions. The early quartz is overgrown by a later generation of quartz that exhibits euhedral termina-tions
Critical minerals in Climax-type magmatic-hydrothermal systems
Today’s global economy is challenged to meet the growing demand for commodities used in existing and emerging advanced technologies. Critical minerals are commodities found in a wide variety of ore deposits that are vital to the economic or national security of individual nations that are vulnerable to supply disruption. The U.S. Geological Survey is striving to advance understanding of critical m
Porphyry Copper Systems of the Boulder batholith, Montana
Systems Approach to Critical Minerals Inventory, Research, and Assessment
Semiquantitative mineralogy results from powder X-ray diffraction (XRD) analyses of mineral scales from The Geysers geothermal field, California, USA
The major, minor, and trace element geochemistry of mineral scales from The Geysers geothermal field, California, USA
Whole rock major, minor, and trace element geochemistry of the upper part of the Mount Emmons-Redwell porphyry molybdenum (Climax-type) deposit, Redwell Basin, Crested Butte, Colorado
Science and Products
Evidence for a high-level porphyritic intrusion below the Sunnyside epithermal vein deposit, Colorado
High-temperature quartz veins were identified in drill core at ~600 m below the Sunnyside epithermal base and pre-cious metal deposit in southwestern Colorado. The veins consist of early anhedral quartz that shows a bluish ca-thodoluminescence emission and hosts heterogenous silicate melt inclusions. The early quartz is overgrown by a later generation of quartz that exhibits euhedral termina-tions
Critical minerals in Climax-type magmatic-hydrothermal systems
Today’s global economy is challenged to meet the growing demand for commodities used in existing and emerging advanced technologies. Critical minerals are commodities found in a wide variety of ore deposits that are vital to the economic or national security of individual nations that are vulnerable to supply disruption. The U.S. Geological Survey is striving to advance understanding of critical m
Porphyry Copper Systems of the Boulder batholith, Montana
Systems Approach to Critical Minerals Inventory, Research, and Assessment
Semiquantitative mineralogy results from powder X-ray diffraction (XRD) analyses of mineral scales from The Geysers geothermal field, California, USA
The major, minor, and trace element geochemistry of mineral scales from The Geysers geothermal field, California, USA
Whole rock major, minor, and trace element geochemistry of the upper part of the Mount Emmons-Redwell porphyry molybdenum (Climax-type) deposit, Redwell Basin, Crested Butte, Colorado
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government