Supplemental Material: Tectonic fractures induced by strike-slip faulting in intracratonic ultradeep carbonate rocks: Insights from the finite element method and self-adaptive constraints computational model for boundary conditions

Table S1 contains the subsections involved, the information needed, how the information was obtained, and the specific section in which the information was applied in this study. Figure S1 contains the relationships between different tectonic stress types and the mechanical properties and occurrence of fractures.