2017
DOI: 10.1016/j.jsames.2017.05.005
|View full text |Cite
|
Sign up to set email alerts
|

Changing fluvial styles in volcaniclastic successions: A cretaceous example from the Cerro Barcino Formation, Patagonia

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
2

Citation Types

0
5
0
2

Year Published

2018
2018
2021
2021

Publication Types

Select...
5
1
1

Relationship

1
6

Authors

Journals

citations
Cited by 16 publications
(7 citation statements)
references
References 68 publications
0
5
0
2
Order By: Relevance
“…: dIVERSITY OF FOSSIL TURTLES IN CHUBUT rich, alluvial successions. The taxa from the Puesto La Paloma Member inhabited ephemeral and unconfined alluvial system that interacted with aeolian dunes and dry interdune zones (de la Fuente et al, 2011;Umazano et al, 2017). Turtles from the Cerro Castaño Member developed within a fluvial scenery, characterized by a permanent, meandering fluvial system, with lacustrine facies and minor ash-fall deposits (Umazano et al, 2017).…”
Section: 1-12)mentioning
confidence: 99%
See 1 more Smart Citation
“…: dIVERSITY OF FOSSIL TURTLES IN CHUBUT rich, alluvial successions. The taxa from the Puesto La Paloma Member inhabited ephemeral and unconfined alluvial system that interacted with aeolian dunes and dry interdune zones (de la Fuente et al, 2011;Umazano et al, 2017). Turtles from the Cerro Castaño Member developed within a fluvial scenery, characterized by a permanent, meandering fluvial system, with lacustrine facies and minor ash-fall deposits (Umazano et al, 2017).…”
Section: 1-12)mentioning
confidence: 99%
“…The taxa from the Puesto La Paloma Member inhabited ephemeral and unconfined alluvial system that interacted with aeolian dunes and dry interdune zones (de la Fuente et al, 2011;Umazano et al, 2017). Turtles from the Cerro Castaño Member developed within a fluvial scenery, characterized by a permanent, meandering fluvial system, with lacustrine facies and minor ash-fall deposits (Umazano et al, 2017). The Bajo Barreal Formation, in the Golfo San Jorge Basin, is characterized by fluvial depositional systems with minor ashfall events, deposited within endorreic basins (Sciutto, 1981;Figari et al, 1999;Umazano et al, 2008;Allard et al, 2015;Paredes et al, 2016).…”
Section: 1-12)mentioning
confidence: 99%
“…The Cerro Barcino Formation of the Chubut Group is composed of fluvial volcaniclastic sediments and comprises four members, from bottom to top: Puesto La Paloma, Cerro Castaño, Las Plumas and Puesto Manuel Arce (Figari et al, 2015;Rauhut et al, 2003;Umazano et al, 2017). The Cerro Castaño Member comprises sheet-to ribbon-channel sandstone bodies intercalated within tuffaceous and fine-grained sediments (Umazano et al, 2017). U-Pb dating of tuffs collected from an ash layer at the titanosaur excavation, a few meters below the plant horizon, indicates an age of ca.…”
Section: Geological Settingmentioning
confidence: 99%
“…The lower section of the Cerro Barcino Formation (Puesto La Paloma Member) mainly records unconfined fluvial sedimentation (e.g. Allard, Paredes, Foix, & Giacosa, 2010;Umazano, Krause, Bellosi, Perez, & Visconti, 2014). The overlying Cerro Castaño Member was deposited by channeled fluvial systems dominated by meandering-like features (e.g.…”
Section: Geological Settingmentioning
confidence: 99%
“…The overlying Cerro Castaño Member was deposited by channeled fluvial systems dominated by meandering-like features (e.g. Umazano et al, 2014). The remaining members of the Chubut Group (Las Plumas, Puesto Manuel Arce and Bayo Overo) crop out eastward, outside the study area, and also record channeled fluvial systems (Codignotto et al, 1978).…”
Section: Geological Settingmentioning
confidence: 99%