Michael T. DeAngelis
This is a likely match — the affiliation was inferred from OpenAlex, ORCID, and web sources but has not been fully confirmed. Treat with appropriate caution.
Associate Professor Director of the School of Physical Sciences
Also affiliated: Colgate University (2005); University of Tennessee at Knoxville (2005–2012)
Research Areas
Links
Biography and Research Information
OverviewAI-generated summary
Michael T. DeAngelis's research investigates geological and environmental processes, with recent work focusing on the analysis of diamond-bearing lamproite and adjacent sediments in Pike County, Arkansas, and mineralization within Arkansas novaculite near Magnet Cove. He has also explored the breakdown of dolomite in high-pressure, high-temperature water conditions. His publications include studies on water quality monitoring in the Lower Arkansas-Maumelle HUC-8 watershed and place-based field experiences in Arkansas. DeAngelis has also contributed to educational research, examining the use of thin section imaging in laboratory settings and adapting face-to-face lectures for online teaching. His work also includes the sol-gel synthesis of nanoscale olivine. DeAngelis holds a h-index of 5, with 51 total publications and 143 total citations.
Metrics
- h-index: 5
- Publications: 38
- Citations: 122
Positions
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Associate Professor Director of the School of Physical Sciences publications 2016–2025University of Arkansas at Little Rock Institution web page
Selected Publications
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LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS (2025)
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FIELD MAPPING AND GEOCHEMICAL ANALYSIS OF DIAMOND-BEARING LAMPROITE AND ADJACENT SEDIMENTS FROM THE WORTHINGTON DIAMOND MINE, PIKE COUNTY, ARKANSAS (2025)
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INTRIGUING MINERALIZATION WITHIN ARKANSAS NOVACULITE ADJACENT TO MAGNET COVE AT THE VARNEDORE PROSPECT, MALVERN, ARKANSAS (2025)
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An experimental study of the breakdown of dolomite in H2O at 700 °C, 100 MPa (2024)
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MAKING FACE-TO-FACE LECTURE TUTORIALS WORK FOR ONLINE TEACHING (2021)
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Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition (2018)
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Oxygen diffusion and exchange in dolomite rock at 700 °C, 100 MPa (2016)
Collaboration Network
Top Collaborators
- Oxygen diffusion and exchange in dolomite rock at 700 °C, 100 MPa
- An experimental study of the breakdown of dolomite in H2O at 700 °C, 100 MPa
- Oxygen diffusion and exchange in dolomite rock at 700 °C, 100 MPa
- An experimental study of the breakdown of dolomite in H2O at 700 °C, 100 MPa
- Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition
- Oxygen diffusion and exchange in dolomite rock at 700 °C, 100 MPa
- MAKING FACE-TO-FACE LECTURE TUTORIALS WORK FOR ONLINE TEACHING
- LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS
- Oxygen diffusion and exchange in dolomite rock at 700 °C, 100 MPa
- Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition
- Surface energy of fayalite and its effect on Fe-Si-O oxygen buffers and the olivine-spinel transition
- INTRIGUING MINERALIZATION WITHIN ARKANSAS NOVACULITE ADJACENT TO MAGNET COVE AT THE VARNEDORE PROSPECT, MALVERN, ARKANSAS
- INTRIGUING MINERALIZATION WITHIN ARKANSAS NOVACULITE ADJACENT TO MAGNET COVE AT THE VARNEDORE PROSPECT, MALVERN, ARKANSAS
- FIELD MAPPING AND GEOCHEMICAL ANALYSIS OF DIAMOND-BEARING LAMPROITE AND ADJACENT SEDIMENTS FROM THE WORTHINGTON DIAMOND MINE, PIKE COUNTY, ARKANSAS
- FIELD MAPPING AND GEOCHEMICAL ANALYSIS OF DIAMOND-BEARING LAMPROITE AND ADJACENT SEDIMENTS FROM THE WORTHINGTON DIAMOND MINE, PIKE COUNTY, ARKANSAS
- LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS
- LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS
- LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS
- LITTLE ROCK ROCKS!: PLACE-BASED FIELD EXPERIENCES IN AND AROUND THE CAPITAL CITY OF ARKANSAS
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