Cholchol Formation | |
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Stratigraphic range: Middle–Upper Miocene | |
Type | Geological formation |
Underlies | Pliocene and Pleistocene alluvial fans and volcaniclastic deposits |
Overlies | Bahía Mansa Metamorphic Complex Coastal Batholith of central Chile Mesozoic sediments |
Thickness | 150–200 m (490–660 ft) |
Lithology | |
Primary | Claystone, sandstone, tuff, calcarenite, calcirudite |
Location | |
Coordinates | 38°00′S 72°00′W / 38.0°S 72.0°W |
Region | Araucanía Region |
Country | Chile |
Type section | |
Named for | Cholchol |
Named by | Floreal García |
Year defined | 1968 |
Cholchol Formation (Spanish: Formación Cholchol) is a geological formation composed of sediments that were deposited during the Miocene in the Temuco Basin of south–central Chile. The sediments were deposited in a marine environment.[1]