The Salt-Gila River, Arizona source of the late Eocene Poway Conglomerate of the San Diego area and the limited offset of the San Andreas fault [abs.]

Lowry, W.D., and Grivetti, R.M., 1979, The Salt-Gila River, Arizona source of the late Eocene Poway Conglomerate of the San Diego area and the limited offset of the San Andreas fault [abs.]: Geological Society of America Abstracts with Programs, v. 11, no. 7, p. 469.

Authors

Lowry, W.D., and Grivetti, R.M.

Publication Date

1979

Citation

Geological Society of America Abstracts with Programs, v. 11, no. 7, p. 469.

State

AZ CA

Province

County

MA GI YU

Placenames

Goldfield Mts.

Tonto Basin

Yuma area

Keywords

Fluvial Sedimentary

Sedimentary Petrology

Plate Tectonics

Faulting

Paleogeography

More Keywords

Fluvial Sedimentary, Sedimentary Petrology, Plate Tectonics, Faulting, Paleogeography, Whitetail Conglomerate(Whitetail Fm) - Oligocene - Whitetail assemblage, Apache Group - Middle Proterozoic, Mazatzal Group - Tonto Basin Supergroup - Early Proterozoic, (Geronimo Head Fm)[Peters Canyon dome complex][Peters Canyon complex] - Miocene,

AzGeoBib RefNum

6163