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Palo Pintado Formation

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Journal Article
Journal: PALAIOS
Published: 24 July 2018
PALAIOS (2018) 33 (7): 338–352.
... Pintado Formation. Traces of arthropod herbivory are found on 303 foliar impressions, 288 from the Palo Pintado Formation and just 15 from the San José Formation. Forty-four percent of all traces were found on Thelypteris interrupta (Willd.) Iwatsuki 1963 (Thelypteridaceae), followed by Cedrela...
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Journal Article
Journal: Geology
Published: 01 March 2010
Geology (2010) 38 (3): 235–238.
... (Eastern Cordillera, northwest Argentina). U-Pb zircon data from ash layers constrain the transition between the finer grained fluvial-lacustrine Palo Pintado Formation and the coarser grained fluvial-alluvial San Felipe Formation to ca. 5.2 Ma and the first deposition of sediment derived from the present...
FIGURES
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A ) Map showing the geoghraphic locations of the <span class="search-highlight">formations</span>.  B ) Landscape...
Published: 24 July 2018
Fig. 1.— A ) Map showing the geoghraphic locations of the formations. B ) Landscape of San José Formation. C ) Landscape of Palo Pintado Formation. D ) Detail of sediment containing fossil impressions from Palo Pintado Formation. Abbreviations: a = Schinus herbstii ; b = Cedrela
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A ) Abundance of recognized functional feeding groups from San José (middle...
Published: 24 July 2018
Fig. 6.— A ) Abundance of recognized functional feeding groups from San José (middle Miocene) and Palo Pintado (late Miocene) formations in northwestern Argentina. The axes represent the occurrence (x) and abundance (y) of FFGs. B ) Comparison of analyzed leaves and damaged leaves. C
Image
A: Stable isotope values of pedogenic carbonate nodules and rodent incisor ...
Published: 01 March 2010
Figure 2. A: Stable isotope values of pedogenic carbonate nodules and rodent incisor enamel plotted as error weighted means (Tables DR3, DR4; for more information, see the Data Repository [see footnote 1 ]). VPDB—Vienna Peedee belemnite. B: Generalized stratigraphy showing Palo Pintado Formation
Journal Article
Journal: PALAIOS
Published: 26 July 2022
PALAIOS (2022) 37 (7): 349–367.
... record, DT103 also is found on Thelypteris interrupta occurring in the Palo Pintado Formation from the late Miocene of Argentina ( Robledo et al. 2015 ), and are assigned to the hole or window feeding ichnotaxon Folifenestra intervenosa . The ichnofossil F. intervenosa could be disrupted DT103...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1961
AAPG Bulletin (1961) 45 (7): 1045–1089.
... at the rate of 3,120 BOPD, gravity 20.2° API, and produces from the Oligocene Mugrosa formations at T.D. 7,790 ft. The previously discovered small pumpers produce from the Eocene La Paz formation, the so-called “Cantagallo sands,” and it appears that the producing Mugrosa sands do not exist on the east...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1955
AAPG Bulletin (1955) 39 (7): 1231–1277.
... , Kenneth E. , and Hugh Dresser , 1954 , “ Contributions to Knowledge of the Brazilian Paleozoic: No. I. A. Introductory Survey of the Brazilian Carboniferous. B. Notes on Some Brachiopods from the Itaituba Formation (Pennsylvanian) of the Tapajos River, Brazil ,” Bull. Amer. Paleon. , Vol. 35...
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Journal Article
Journal: AAPG Bulletin
Published: 01 July 1962
AAPG Bulletin (1962) 46 (7): 1077–1140.
... an interval of “Horizonte Canadon Seco-1” which is the normal productive formation of Kohuel Kaike. This successful completion extends considerably the proved productive area of this zone. Well 0–121 was completed with an initial production of 151 BPD from the upper part of the Chubutiano Formation...
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Journal Article
Journal: GSA Bulletin
Published: 26 April 2022
GSA Bulletin (2023) 135 (1-2): 81–103.
... strike to the NE (Quebrada del Toro) in the Agujas Conglomerate and dated by U-Pb zircon on tuff layers between ca. 10 and 8 Ma ( DeCelles et al., 2011 ). Sedimentation continued with the <9 Ma deposition of the Palo Pintado Formation ( Carrapa et al., 2012 ; Pingel et al., 2016 ). Paleocurrent data...
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Journal Article
Journal: PALAIOS
Published: 01 February 2005
PALAIOS (2005) 20 (1): 51–63.
... in Valle Pintado, located in the southern part of the Ischigualasto Formation within the Ischigualasto Provincial Park and World Heritage Site. Figure 1 is a stratigraphic section applicable to the site. The sedimentary facies shown were identified according to the criteria of Miall (1977) . The 3-meter...
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Series: Geological Society, London, Special Publications
Published: 01 January 2013
DOI: 10.1144/SP377.2
EISBN: 9781862396388
... ) form the Metán Subgroup. The Jujuy Subgroup corresponds to the upper part of synorogenic sediments, which consists of the alluvial conglomerates of the San Felipe Formation and the Piquete Formation, the sandstones and shales of the Palo Pintado Formation, and the sandstones and conglomerates...
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