Supplemental Material: Co-inversion of multiple thermochronometers and a paleomagnetic thermometer at a Columbia River flood basalt feeder dike (Oregon, USA) demonstrates the sensitivity of thermal history results to diverse data constraints

Supplemental tables include detailed thermochronology and isotope data. Supplemental figures include autocorrelation, bivariate covariance, model age versus observed age, and age versus effective uranium plots. Supplemental text includes more detailed explanations of the 1-D thermal model used in the inversion, sensitivity testing of our apatite fission-track annealing model, and choices made to initialize the model.