Implications of perennial saline springs for abnormally high fluid pressures and active thrusting in western California
- Univ. of California, Davis (United States)
Perennial saline springs in the Rumsey Hills area, southwestern Sacramento Valley, California, locally discharge at high elevations and near ridgetops. The springs are cold, are commonly associated with natural gas seeps, and typically emerge along west-vergent thrust faults. Stable isotope analyses indicate that the spring waters are similar to oil-field formation fluids and they have had a significant residence time in the subsurface at moderate temperatures. The nonmeteoric character of the springs demonstrates that they are not being fed by perched water tables. The authors propose that these subsurface formation waters are being forced to the surface by anomalously high porefluid pressures. The Rumsey Hills area is one of Quaternary uplift, thrusting, and crustal shortening, and prospect wells drilled there have encountered anomalously high fluid pressures at shallow depths. They attribute these high fluid pressures to active tectonic compression and shortening of Cretaceous marine sedimentary rocks. The widespread occurrence of anomalously high pore-fluid pressures and perennial saline springs in the Coast Ranges and western Great Valley suggests that much of western California may be characterized as a seismically active, overpressured thrust belt. The emergence of formation waters along thrust faults further suggests that patterns of subsurface fluid flow in western California may be similar to those in overpressured accretionary prisms, and that excess fluid pressures may also play a role in the distribution of seismicity.
- OSTI ID:
- 6952025
- Journal Information:
- Geology; (United States), Vol. 20:5; ISSN 0091-7613
- Country of Publication:
- United States
- Language:
- English
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Related Subjects
ARTESIAN BASINS
GEOLOGIC FAULTS
HYDROLOGY
CALIFORNIA
FLUID FLOW
GEOCHEMISTRY
GROUND WATER
MINERAL SPRINGS
PORE PRESSURE
SEEPS
SEISMICITY
SEISMOLOGY
WATER CHEMISTRY
CHEMISTRY
DEVELOPED COUNTRIES
GEOLOGIC FRACTURES
GEOLOGIC STRUCTURES
HYDROGEN COMPOUNDS
NORTH AMERICA
OXYGEN COMPOUNDS
USA
WATER
WATER SPRINGS
580000* - Geosciences