Zapata Formation
Zapata Formation Stratigraphic range: Lower Cretaceous | |
---|---|
Type | Geological formation |
Underlies | Punta Barrosa Formation |
Overlies | Tobífera Formation |
Lithology | |
Primary | Shale |
Location | |
Region | Magallanes y la Antártica Chilena Region |
Country | Chile |
Zapata Formation (Spanish: Formación Zapata) is a sedimentary formation of Lower Cretaceous age. Much of the formation is folded and faulted as consequence of the Andean orogeny.[1] In the outcrops of Zapata Formation near Torres del Paine the southernmost fossil of the ichthyosaur species Platypterygius has been found.[2]
References
- ↑ Fildani, Andrea, Romans, B.W., Fosdick, J.C., Crane, W.H., and Hubbard, S.M. (2008). Orogenesis of the Patagonian Andes as reflected by basin evolution in southernmost South America, in Spencer, J.E., and Titley, S.R., eds., Ores and orogenesis: Circum-Pacific tectonics, geologic evolution, and ore deposits: Arizona Geological Society Digest 22: 259-268.
- ↑ Pardo-Pérez, Judith; Frey, Eberhard; Stinnesbeck, Wolfgang; Fernández, Marta S.; Rivas, Luis; Salazar, Christian; Leppe, Marcelo (2012). "An ichthyosaurian forefin from the Lower Cretaceous Zapata Formation of southern Chile: implications for morphological variability within Platypterygius" (PDF). Palaeoclimate, Palaeobiology, Paleoenvironments. 92: 287–294. doi:10.1007/s12549-012-0074-8. Retrieved 30 August 2016.
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