Tectonics, Sedimentary Basins, and Provenance: A Celebration of the Career of William R. Dickinson
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Paleogeographic and paleotectonic setting of the Middle Miocene Mint Canyon and Caliente Formations, southern California: An integrated provenance study
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Published:December 28, 2018
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CiteCitation
Johanna F. Hoyt, Kevin T. Coffey, Raymond V. Ingersoll, Carl E. Jacobson, 2018. "Paleogeographic and paleotectonic setting of the Middle Miocene Mint Canyon and Caliente Formations, southern California: An integrated provenance study", Tectonics, Sedimentary Basins, and Provenance: A Celebration of the Career of William R. Dickinson, Raymond V. Ingersoll, Timothy F. Lawton, Stephan A. Graham
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ABSTRACT
Conglomerate-clast analysis, sandstone petrology, and detrital zircon age data determine the provenance and correlation of the Middle Miocene Mint Canyon and Caliente Formations. Detrital zircon age assemblages and sandstone compositions confirm that the Mint Canyon Formation is the upstream equivalent of the southern Caliente Formation and that both are dissimilar to the Punchbowl Formation. The Mint Canyon and Caliente Formations are remnants of an axial drainage system that was likely confined by the ancestral Sierra Pelona/Blue Ridge to the north and ancestral San Gabriel Mountains to the south; sediments derived from these local highlands dominate in the Mint Canyon...
- absolute age
- basins
- California
- Cenozoic
- clastic rocks
- conglomerate
- dates
- drainage basins
- middle Miocene
- Miocene
- Neogene
- nesosilicates
- orthosilicates
- paleogeography
- Pelona Schist
- provenance
- Punchbowl Formation
- San Gabriel Mountains
- sediment transport
- sedimentary basins
- sedimentary rocks
- silicates
- Southern California
- tectonics
- Tertiary
- transport
- U/Pb
- United States
- upper Miocene
- zircon
- zircon group
- Caliente Formation
- Mint Canyon Formation
- Sierra Pelona
- detrital zircon