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Marine Incursions: Implications for crustal thinning and regional strain. Kristin McDougall U.S. Geological Survey Flagstaff, Arizona 86001 kris@usgs.gov with assistance from Ana Luisa Carreno, Rebecca Dorsey, Arturo Martin, and Michael Oskin. Questions. Number of incursions Age Extent
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Marine Incursions: Implications for crustal thinning and regional strain Kristin McDougall U.S. Geological Survey Flagstaff, Arizona 86001 kris@usgs.gov with assistance from Ana Luisa Carreno, Rebecca Dorsey, Arturo Martin, and Michael Oskin
Questions • Number of incursions • Age • Extent • Environment
Locations • Lower Colorado River • Salton Trough • Gulf of California
Correlation lower Colorado River, Salton Trough, and Gulf of California
Middle Miocene microfossils • Range of reworked planktic foraminifers or calcareous nannofossils
Age diagnostic Middle Miocene Taxa Sections • Hermosillo/Guaymas • Cerro Prieto • Fish Creek • Whitewater/Cabazon • Laguna Salada • San Felipe • Tres Marias Islands
Middle Miocene microfossils • Range of reworked planktic foraminifers or calcareous nannofossils
Correlation lower Colorado River, Salton Trough, and Gulf of California
Gulf of California Late Miocene ~ 6-8 MaPlio-Pleistocene <5.3 Ma
Salton Trough Late Miocene ~ 6-8 Ma Plio-Pleistocene < 5.3 Ma
Questions • Number of incursions • Age • Extent • Environment
Middle Miocene incursion • 11-14 Ma • In situ faunas suggest this incursion extends at least as far north as the Hermosillo and Guaymas • Reworked microfossils found further north. • The age of the sediments middle Miocene faunas are reworked in to becomes older to the north. • Northern limit of this incursion has not been determined. • Deposition occurred during warm climatic conditions and high sea level.
Late Miocene incursion • 6-7 Ma • Extends as far north as San Gorgonio Pass, California, and as far east as Yuma, Arizona. • Wide variety of environments in a warm climatic interval and high sea level
Plio-Pleistocene incursion • Post 5.3 Ma • Extends throughout most of the Salton Trough and lower Colorado River region as well as the current Gulf of California. • The marine section was strongly affected by the Colorado River, which rapidly filled the area with fresh water and sediment, reducing the marine influence • Wide variety of depositional environments