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Goldsby DL, Tullis TE. Flash heating leads to low frictional strength of crustal rocks at earthquake slip rates. Science. 2011;334(6053):216-8doi: 10.1126/science.1207902.
Goldsby, D. L., & Tullis, T. E. (2011). Flash heating leads to low frictional strength of crustal rocks at earthquake slip rates. Science (New York, N.Y.), 334(6053), 216-8. https://doi.org/10.1126/science.1207902
Goldsby, David L, and Tullis, Terry E. "Flash heating leads to low frictional strength of crustal rocks at earthquake slip rates." Science (New York, N.Y.) vol. 334,6053 (2011): 216-8. doi: https://doi.org/10.1126/science.1207902
Goldsby DL, Tullis TE. Flash heating leads to low frictional strength of crustal rocks at earthquake slip rates. Science. 2011 Oct 14;334(6053):216-8. doi: 10.1126/science.1207902. PMID: 21998385.
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