INTRODUCTION
| Motivation and objectivesCorrectly identifying sediment source areas plays a key role in reconstructing paleogeography, testing tectonic models, correlating surface-subsurface stratigraphy, and predicting the distribution of source, seal, and reservoir. Traditional approaches to sediment source analyses rely on petrographic, geochemical, or isotopic analysis on tracers (e.g. Zircon U-Pb age, lithologic compositions) (Dickinson, 1985;