|Basin Fill Sandstone and Carbonate Aquifers, Basin and Range
(Arizona, Nevada, and California)
Sand-body continuity of the Tertiary basin-fill aquifers is inferred from data in Planert (1996), and Robson (1996). Sand-body continuity in these aquifers is typically very high within each fault-bounded basin, but poor between basins because of the complex structure.
Planert, M., 1996, Ground water atlas of the United States, Segment 1: California and Nevada: U.S. Geological Survey Atlas.
Robson, S. G., 1996, Ground water atlas of the United States, Segment 2: Colorado, Nevada, and New Mexico: U.S. Geological Survey Atlas.