Tables S1 to S5: A data-driven approach to understanding the relations between geothermal exploration parameters: insights from Coso, Brady and Desert Peak, USA

Table S1. The K–S test result. The null hypothesis was rejected in most cases, showing that the distributions of datasets are primarily different.
Table S2. The p-values of the coefficients and intercepts from the linear regression models of Fault Density Maps fit by Mineral Density Maps.
Table S3. The p-values of the coefficients and intercepts from the linear regression models of Multiclass Temperature Maps fit by Fault Density Map and Mineral Density Maps.
Table S4. The AIC values from the regression models of Fault Density Maps fit by Mineral Density Maps.
Table S5. The AIC values from the regression models of Multiclass Temperature Maps fit by Fault Density Map and Mineral Density Maps.