... in the pioneering studies by Kayser during the latest 19 th century and by Kobayashi and Harrington during the 1930s, which are still in need of revision. The brachiopods described in this study occur in the Saladillo Formation exposed along the footpath to the Parcha locality, between Angosto de Lampazar...

...Figure 1. A: Geologic map of North Calchaquí Valley. B: Columns of Quebrada de los Colorados Formation in Saladillo and La Poma; schematic facies stacking is represented. C: Syntectonic angular unconformity between sequences I and II. Stereoplot shows poles to bedding in both sequences. D: Geology...

... Papa et al. , 2013 ), as well as the underlying post-rift sequences (Maíz Gordo Formation, MG, Marquillas et al. , 2005 ). Fig. 1. (a) Location and geological map of the northern Calchaquí Valley. (b) Geological map of the Saladillo area. (c) Detailed geological map of the Saladillo area...

...; A  =  Anta Formation, geology taken from Seggiaro and others, 1997 ). (D) Average rainfall between 2000 and 2005, inclusive; meteorological station located 30 km north from landslide site, in similar geomorphic and climatic situation. The Subandean Ranges in northwestern Argentina (22–26°S...

...Figure 2 —Generalized stratigraphic column of Famatina Group beds exposed in the Cachiyuyo River area (left), and detail of the sampled interval of the Molles Formation (right) showing position of brachiopod-bearing levels. CA: Cachiyuyo River section; QS: Saladillo Chico River section; S...

... unconformably over Sequence III beds ( B ossi et alii, 2001 ). The basal beds of the Cenozoic succession correspond to the Saladillo Formation and outcrop in the El Remate area ( figs. 3 , 5 ) of the Amaicha Valley. Fine-grained red sands and siltstone intercalated with laminated gypsum overlie...

...Fig. 10 View of the NE-striking Saladillo fault system. About 800 m of Abanico Formation pyroclastic rocks were accumulated in a tectonic basin to the northwest of the fault system. The same structures were later reactivated as dextral-reverse faults and controlled the emplacement of andesitic...

... of an anomalously hot mantle that reflects thinning of the regional lithosphere and volcanism. Further analyses of the distribution of calcrete show they are carbonate-rich fluvial terraces, whose formation is controlled by the response of the river network to regional uplift and climate. Supplementary Materials...

.... The Tremadoc is particularly well exposed in this area and is represented in ascending order by the Cardonal, Saladillo, and Parcha Formations. The ostracods mainly occur within the lower part of the Parcha Formation. This formation conformably overlies the Saladillo Formation. The base of the Parcha Formation...

... Salta Province 4 Saladillo Formation Coquena Formation B1 B2 W1 W2 Ba MN1 CS IC A1 A1 A1 A1 A2 A2 A2 A2 A2 LINGULOIDEA Broeggeria + + Divobolus + + Elliptoglossa + Elkanisca...

..., Lampazar, Cardonal, Devendeus, Saladillo, and Parcha formations ( Fig. 2 ) uncomformably overlying Cambrian rocks of the Meson Group (Keidel, 1943 ; Harrington and Leanza, 1957 ; Astini, 2003 ). The studied locality is nearly 4,000 m in elevation, at a tributary creek...

... west of Southam, Warwickshire, England (Y. G., unpub. data). De la Puente & Rubinstein ( 2009 ) described Lagenochitina from the Aorograptus victoriae graptolite Zone (Saladillo Formation), and chitinozoans from the lower Parsha Formation, Argentina. Chen, Paris & Zhang...

... ). Sedimentation in the Santa María basin started with deposition of 300- m-thick fluvial sandstones of the Saladillo Formation. This unit is overlain by the mid- Miocene to Pliocene Santa María Group ( Galván and Ruiz Huidobro, 1965 ; Bossi and Palma, 1982 ), which has a maximum total thickness of 6200 m...

... from the upper Floian San José Formation of southern Peru (Gutiérrez-Marco et al., 2008 ). The slightly younger A. famatiniana n. sp. occurs in volcaniclastic rocks of the Famatina Range of middle-late Dapingian age. In Anglesey (northwestern Wales), Ahtiella is represented by A. quadrata Bates...