Reference 3034
Sarna-Wojcicki, Andrei M; Bowman, H R; Meyer, C E; Russell, P C; Woodward, M J; McCoy, Gail; Rowe, J J, Jr; Baedecker, P A; Asaro, Frank; Michael, Helen (1984) U. S. Geological Survey Professional Paper, Report: P 1293, 40 pp., 1984
| Authors | Sarna-Wojcicki, Andrei M; Bowman, H R; Meyer, C E; Russell, P C; Woodward, M J; McCoy, Gail; Rowe, J J, Jr; Baedecker, P A; Asaro, Frank; Michael, Helen |
|---|---|
| Year | 1984 |
| Source | U. S. Geological Survey Professional Paper, Report: P 1293, 40 pp., 1984 |
| Pages | 40 pp. |
| Publisher | U. S. Geological Survey, Reston, VA, United States USA |
| ISSN | 1044-9612 |
| GeoRef | 1984-019557 |
| Keywords | Bishop Tuff; California; Cenozoic; Central California; chemical composition; correlation; geochemistry; geochronology; glasses; igneous rocks; Imperial County California; Inyo County California; Mono County California; Neogene; Pearlette Volcanic Ash; Pleistocene; Pliocene; pyroclastics; Quaternary; Riverside County California; San Bernardino County California; San Diego County California; Southern California; tephrochronology; Tertiary; United States; upper Pliocene; USGS; Ventura County California; volcanic ash; volcanic glass; volcanic rocks |
Abstract
Tephra layers volcanic ash and tuff beds of late Cenozoic age in east-central and southern California are identified and correlated by the chemical composition of volcanic glass, stratigraphic criteria, and petrographic characteristics. Among widespread tephra units identified are the Lava Creek ash bed 0.62 m.y., the Bishop ash bed 0.73 m.y., and the Huckleberry Ridge ash bed 2.01 m.y.. All three are identified for the first time in marine strata. Identification of these and other tephra units permits correlation of upper Cenozoic sedimentary strata deposited in marine, fluvial, and lacustrine environments and helps reconcile provincial marine and continental biostratigraphic chronologies.
49 samples from this reference
| Sample | Rock name | Major | Trace | Isotope |
|---|---|---|---|---|
| 1 | Rhyolite | yes | yes | |
| 2 | Pyroclastic-fall | yes | yes | |
| 3 | Pyroclastic-fall | yes | yes | |
| 4 | Pyroclastic-fall | yes | yes | |
| 5 | Pyroclastic-fall | yes | yes | |
| 6 | Pyroclastic-fall | yes | yes | |
| 7 | Pyroclastic-fall | yes | ||
| 8 | Pyroclastic-fall | yes | yes | |
| 9 | Pyroclastic-fall | yes | ||
| 10 | Pyroclastic-fall | yes | yes | |
| 11 | Pyroclastic-fall | yes | yes | |
| 12 | Pyroclastic-fall | yes | yes | |
| 13 | Pyroclastic-fall | yes | ||
| 14 | Tuff | yes | yes | |
| 15 | Pyroclastic-fall | yes | ||
| 17 | Pyroclastic-fall | yes | yes | |
| 18 | Pyroclastic-fall | yes | yes | |
| 19 | Pyroclastic-fall | yes | yes | |
| 20 | Pyroclastic-fall | yes | ||
| 21 | Pyroclastic-fall | yes | yes | |
| 22 | Pyroclastic-fall | yes | yes | |
| 23 | Pyroclastic-fall | yes | yes | |
| 24 | Pyroclastic-fall | yes | yes | |
| 25 | Pyroclastic-fall | yes | yes | |
| 26 | Pyroclastic-fall | yes | ||
| 27 | Pyroclastic-fall | yes | yes | |
| 28 | Pyroclastic-fall | yes | ||
| 29 | Pyroclastic-fall | yes | ||
| 30 | Pyroclastic-fall | yes | ||
| 31 | Pyroclastic-fall | yes | ||
| 32 | Pyroclastic-fall | yes | ||
| 33 | Pyroclastic-fall | yes | yes | |
| 34 | Pyroclastic-fall | yes | yes | |
| 35 | Pyroclastic-fall | yes | yes | |
| 36 | Pyroclastic-flow | yes | yes | |
| 37 | Pyroclastic-fall | yes | ||
| 38 | Pyroclastic-fall | yes | ||
| 41 | Pyroclastic-fall | yes | yes | |
| 43 | Pyroclastic-fall | yes | yes | |
| 44 | Pyroclastic-fall | yes | yes | |
| 45 | Pyroclastic-fall | yes | yes | |
| 46 | Pyroclastic fall | yes | yes | |
| 47 | Pyroclastic fall | yes | ||
| 48 | Pyroclastic fall | yes | yes | |
| 49 | Pyroclastic-fall | yes | yes | |
| 50 | Rhyolite | yes | ||
| 51 | Pyroclastic-fall | yes | yes | |
| 52 | Pyroclastic-fall | |||
| 53 | Pyroclastic-fall |