Fluvial siliciclastic rocks bracketing the Cretaceous-Paleogene (K-Pg) boundary in San Juan Basin, New Mexico (USA), provide records of regional fluvial and tectonic evolution during Laramide orogeny. Petrographic analyses sandstones from Upper Cretaceous Fruitland Formation Kirtland Paleocene Ojo Alamo Sandstone Nacimiento show that rivers depositing these sediments were sourced areas where un...