In this article, we want to explore the topic of Huitrera Formation and delve into its importance in today's society. Huitrera Formation is a concept that has captured the attention of many people in recent years, and its relevance extends to different areas of daily life. From its impact on mental health to its influence in the workplace, Huitrera Formation has proven to play a significant role in the way we face the challenges and opportunities that arise in our daily lives. Through this article, we will seek to analyze different perspectives on Huitrera Formation and its impact on our society, offering a detailed analysis that invites reflection and debate on this currently crucial topic.
| Huitrera Formation | |
|---|---|
| Stratigraphic range: Early Eocene (Casamayoran) | |
| Type | Geological formation |
| Underlies | Collón Curá Formation |
| Overlies | Angostura Colorada Formation |
| Thickness | Up to 1,300 m (4,300 ft) |
| Lithology | |
| Primary | Mudstone, sandstone |
| Other | Andesites, dacitic & rhyolitic ignimbrites, volcanic breccias, tuffs & trachybasalts |
| Location | |
| Coordinates | 41°00′S 71°12′W / 41.0°S 71.2°W |
| Approximate paleocoordinates | 43°30′S 61°12′W / 43.5°S 61.2°W |
| Region | Neuquén & Río Negro Provinces |
| Country | Argentina |
| Extent | Neuquén Basin |
| Type section | |
| Named for | Cerro Huitrera |
| Named by | Ravazzoli & Sesana |
| Year defined | 1977 |
The Huitrera Formation is a geological formation in the Neuquén Basin in northern Patagonian Argentina whose strata date back to the Early Eocene of the Paleogene, or Casamayoran in the South American land mammal age classification.
The formation is together with the Reyhuau basalts part of the Pilcaniyeu Belt, a volcanic belt active in Paleocene to middle Eocene times.[1]
The Huitrera Formation was first defined by Ravazzoli and Sesana in 1977. The name has been used to identify various volcaniclastic sequences, among others in the Ñirihuau fold-and-thrust belt.[2] The up to 1,300 metres (4,300 ft) thick formation comprises mudstones and sandstones deposited in a crater lake environment. Part of the formation comprises andesites, dacitic and rhyolitic ignimbrites, volcanic breccias, tuffs and trachybasalts.[3]
The formation was initially described as Late Eocene to Early Oligocene, but was later dated to 54.24 ± 0.45 Ma, meaning the Huitrera Formation is Ypresian, or in the SALMA classification, Casamayoran in age.
The following macrofossils were reported from the formation:[4]
The formation has also provided many pollen, analyzed in 2003 by Melendi et al.[12]