Skip to main content
U.S. Department of Energy
Office of Scientific and Technical Information

Thermal evolution of coastal California with implications for hydrocarbon maturation

Thesis/Dissertation ·
OSTI ID:6275747
The thermal constraints imposed by plate subduction, cooling oceanic lithosphere, and the migration of a fault-fault-trench triple junction are numerically modeled using finite differences in order to better understand the thermal evolution of coastal California. Numerical solutions for steady state heat transfer are used to estimate the effect of plate subduction in lowering temperatures in coastal California. Numerical solutions for time dependent heat transfer estimate the thermal effect of the passage of the Mendocino triple junction with consequent upwelling of asthenosphere. Calculated heat flow values from the models result in a heat flow distribution similar to measured values from north of Cape Mendocino to the Garlock fault zone. When the calculated paleotemperatures are applied to the Pismo Basin, the basal 300 meters of source rocks are predicted to have entered or be near the liquid oil window. Trends suggested by the thermal models indicate that the more southern basins and basins closer to the North American plate Pacific plate boundary have experienced higher paleotemperatures. Consequently, these basins potentially contain a greater amount of generated hydrocarbons.
Research Organization:
Wyoming Univ., Laramie (USA)
OSTI ID:
6275747
Country of Publication:
United States
Language:
English

Similar Records

Thermal evolution of coastal california with application to hydrocarbon maturation
Journal Article · Sun Sep 01 00:00:00 EDT 1985 · AAPG Bull. (See CODEN: AAPGB); (United States) · OSTI ID:6276075

Thermal and hydrocarbon maturation models for coastal California
Conference · Thu Jan 31 23:00:00 EST 1985 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:6000423

Seismicity and crustal structure at the Mendocino triple junction, Northern California
Technical Report · Mon Nov 30 23:00:00 EST 1998 · OSTI ID:6505