A THREE-DIMENSIONAL GEOLOGIC MAP OF THE SAN JOAQUIN BASIN, CALIFORNIA
The 3-D map spans 370 x 135 km, oriented along the basin axis, and extends to ~17 km depth. Mapped surfaces include the Mesozoic crystalline basement; Cretaceous, Paleocene, Eocene, and Oligocene strata; several Miocene-aged units (which form both petroleum source and reservoir rocks) and Pliocene deposits. Data for these rock units are derived from well logs and seismic reflection lines. The 3-D geologic map shows that Mesozoic basement crops out on the basins eastern margin in the Sierra Nevada, then plunges westward to more than 16 km depth approaching the basins western edge. Although rocks of Jurassic and lower Cretaceous age crop out in the bordering Coast Ranges, these are not found beneath the SJB itself. Instead, upper Cretaceous rocks lie conformably on the basement surface and extend over the northern 2/3rds of the basin. The Eocene Kreyenhagen Formation and Domengine Sandstone form laterally continuous surfaces over much of the basin. Pliocene and Miocene-aged rocks dominate the southern half of the basin area. Differences in rock distribution may reflect tectonism, erosional events, and/or shifting sediment depocenters within the SJB. A series of northwest-southeast trending anticlines on the western margin of the basin extend from the ground surface to Eocene-aged strata, but do not involve Cretaceous-aged rocks, constraining the timing, duration, and style of folding.
The 3-D geologic map of the SJB is the foundation for USGS petroleum systems modeling and resource assessment. This map may also be useful for modeling other geologic processes, such as seismic wave propagation and tectonic strain accumulation on basin-bounding faults.