Thomas M. Mitchell

Seismological Laboratory
University College London (United Kingdom)
Lecturer (assistant professor)

Expertise: Experimental Rock Deformation, Fluid flow, fault damage, earthquake field geology
 
 
About Me Publications
Dorsey, M. T., Rockwell, T. K., Girty, G. G., Ostermeijer, G. A., Browning, J., Mitchell, T. M., & Fletcher, J. M. (2020). Evidence of hydrothermal brine circulation driving elemental mass redistribution in an active fault zone. J. Structural Geology, (accepted). SCEC Contribution 10037
Mitchell, T. M. (2019, 08). What is a FZ? Spatial and temporal variations in crustal fault zone structure and associated properties. Oral Presentation at 2019 SCEC Annual Meeting. SCEC Contribution 9922
Dorsey, M. T., Rockwell, T. K., Girty, G. H., Ostermeijer, G., Mitchell, T. M., & Fletcher, J. M. (2017, 08). Evidence of Na- and Mg-rich Hydrothermal Brines Driving Chloritization and Albitization in an Active Fault Zone: Case Study of the Borrego Fault, Baja CA, Mexico. Poster Presentation at 2017 SCEC Annual Meeting. SCEC Contribution 7839
Fletcher, J. M., Teran, O. J., Rockwell, T. K., Oskin, M. E., Hudnut, K. W., Spelz, R. M., Lacan, P., Dorsey, M. T., Ostermeijer, G., Mitchell, T. M., Akciz, S. O., Hernandez-Flores, A., Hinojosa, A., Peña-Villa, I., & Lynch, D. K. (2020). An analysis of the factors that control fault zone architecture and the importance of fault orientation relative to regional stress. GSA Bulletin, 132(9-10), 2084-2104. doi: 10.1130/B35308.1. SCEC Contribution 10004

Last updated Nov 25, 2020.