Earth:Ranquil Formation
| Ranquil Formation Stratigraphic range: Miocene–Pliocene | |
|---|---|
| Type | Geological formation |
| Underlies | Tubul Formation |
| Overlies | Lebu Group |
| Lithology | |
| Primary | Conglomerate with clay and silt matrix, breccia, sandstone, siltstone, mudstone |
| Other | Conglomerate with sand matrix |
| Location | |
| Coordinates | [ ⚑ ] : 37°36′S 73°42′W / 37.6°S 73.7°W |
| Paleocoordinates | [ ⚑ ] 37°54′S 71°24′W / 37.9°S 71.4°W |
| Region | Bío Bío Region |
| Country |  Chile |
| Type section | |
| Named for | Caleta Ranquil |
| Named by | Juan Tavera |
| Year defined | 1942 |
  Ranquil Formation (Chile) | |
The Ranquil Formation (Spanish: Formación Ranquil) is a Miocene and Pliocene sedimentary formation located in Arauco Province in south–central Chile, including outcrops in Mocha Island. The formation has its greatest thicknesses in the south-west, where its sediments were largely deposited in marine conditions. It overlies unconformably sedimentary formations of the Paleocene-Eocene Lebu Group.[1] The formation is part of the fill of Arauco Basin which is a sedimentary basin that extends south of Concepción.[2]
Macrofossils of the formation are similar to those of Navidad (34° S) and Lacui Formations (43° S), two nearby Miocene marine formations.[3]
The base of the Ranquil Formation is the so-called "main unconformity", which is thought to have been formed by erosion during a period of tectonic inversion.[4]
The formation was first defined in 1942 by Juan Tavera.[1]
Units
The formation has been subdivided into five units, with the lowermost being made up of sandstone and shale, and the second lowest one being made up of a conglomerate. The middle unit is made up of mudrock and massive sandstone. At some places the middle unit is overlain by a unit made up of sandstone with thin layers of conglomerate and sandstone that has been bioturbated. The uppermost unit include a breccia and the so-called Huenteguapi sandstone.[2] The sediments of Huenteguapi sandstone evidences that a megatsunami struck the coast of south–central Chile in the Pliocene,[2] which has been linked to the hypothetical Eltanin impact.
Fossil content
The Ranquil Formation contains the following trace fossils: Zoophycos, Chondrites, Phycosiphon, Nereites missouriensis, Lockeiasiliquaria, Parataenidium, Ophiomorpha, Rhizocorallium and possibly also Psammichnites.[5]
See also
References
- ↑ 1.0 1.1 García A., Floreal (1968). Ceccioni, Giovanni. ed (in es). El Terciario de Chile Zona Central. Santiago de Chile: Ediorial Andrés Bello. pp. 25–57.
- ↑ 2.0 2.1 2.2 Le Roux, J.P.; Nielsen, Sven N.; Kemnitz, Helga; Henriquez, Álvaro (2008). "A Pliocene mega-tsunami deposit and associated features in the Ranquil Formation, southern Chile". Sedimentary Geology 203 (1): 164–180. doi:10.1016/j.sedgeo.2007.12.002. Bibcode: 2008SedG..203..164L. http://repositorio.uchile.cl/bitstream/handle/2250/125260/Le%20Roux_J_P.pdf?sequence=1. Retrieved 11 April 2016.
- ↑ Finger, Kenneth L.; Nielsen, Sven N.; Devries, Thomas J.; Encinas, Alfonso; Peterson, Dwan E. (2007). "Paleontologic evidence for sedimentary displacement in Neogene forearc basins of Central Chile". PALAIOS 22 (1): 3–16. doi:10.2110/palo.2005.p05-081r. Bibcode: 2007Palai..22....3F. http://www.ucmp.berkeley.edu/people/klf/KLF_files/Palaios.pdf. Retrieved 28 July 2016.
- ↑ Becerra, Juan; Contreras-Reyes, Eduardo; Arriagada, César (2013). "Seismic structure and tectonics of the southern Arauco Basin, south-central Chile (~ 38°S)". Tectonophysics 592: 53–66. doi:10.1016/j.tecto.2013.02.012. Bibcode: 2013Tectp.592...53B.
- ↑ Le Roux, Jacobus P.; Nielsen, Sven N.; Henríquez, Álvaro (2008). "Depositional environment of Stelloglyphus llicoensis isp. nov.: a new radial trace fossil from the Neogene Ranquil Formation, south-central Chile". Revista Geológica de Chile 35 (2): 307–319. doi:10.5027/andgeov35n2-a06. http://www.scielo.cl/scielo.php?script=sci_arttext&pid=S0716-02082008000200006. Retrieved 29 July 2016.
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