San Diego State University
College of Sciences
Department of Geological Sciences
Home About Us Undergraduate Students Graduate Students Faulty and Staff Research Outreach How You can Help Us

Department Blog

Blackboard at Geological Sciences

SDSU WebPortal

Department of Geological Sciences Webinar
3-D seismic, well log, and petrographic analyses of the Victoria Island structure, a potential buried impact crater, San Joaquin county, California
Jared Morrow
Department of Geological Sciences
San Diego State University
Bennett Spevack
ABA Energy Corporation
Bakersfield

Web Movie
FullscreenSpacePodcast downloadSpace CommentsSpaceBlog
Bridget Smith-Konter
Analyses of a 3-D seismic survey and well logs in the southwestern Sacramento basin, San Joaquin County, California, have revealed a subsurface, circular, ~5.5-km-diameter anomaly that may represent a previously unrecognized complex impact crater. This unique anomaly, buried 1,490–1,600 m below sea level under the southwestern part of the Sacramento-San Joaquin Delta, is provisionally named the Victoria Island structure for an overlying surface geographic feature.
The Victoria Island structure is characterized by a concentric, annular, terraced rim and trough surrounding a structurally uplifted central peak. Well logs tied to seismic data show that the upper surface of the structure occurs stratigraphically near the top of the siliciclastic, continental to shallow-marine Domengine Formation, indicating a middle Eocene age. Overlying fill material, which reaches an estimated thickness of at least 80 m in the trough, is primarily deep-marine, middle Eocene Nortonville Shale. Both well and seismic data indicate thinned Domengine and thickened Nortonville sections across the center of the feature. A disturbed stratigraphic sequence under the structure includes upper to lower Domengine and underlying lower Eocene Capay Formation and Cretaceous-Paleocene Mokelumne River Formation siliciclastic units. Characterized by discontinuous seismic reflectors, the central peak is estimated to be ~600 min diameter with at least 35 m of structural uplift. The seismic data demonstrate that the feature is ‘rootless’, being underlain by gently dipping, relatively undeformed strata. The 3-D data further suggest the presence of a series of discontinuous, inward dipping, concentric normal faults with minor offset surrounding the trough and outer rim areas. Estimates of the dimensions of the structure indicate a circularity ratio (short-to-long axes) of 0.91 and a depth-todiameter ratio of ~0.02.
5500 Campanile Dr • 237 Geology Mathematics and Computer Science Building  • San Diego • CA 92182-1020 • (619) 594-5586