
handle: 11336/39914
En el flanco oriental de la Sierra de Pedernal la estratigrafía del Paleozoico Inferior es compleja y está afectada por un intenso tectonísmo. En el presente trabajo se describe un nuevo perfl en el que se reconocen por primera vez para esta región, suprayaciendo a la Formación San Juan, relictos de las formaciones Los Azules y Don Braulio, así como una espesa sucesión de la Formación Rinconada. Este hallazgo permite extender la distribución paleogeográfica de las cuencas darriwiliana e hirnantiana hacia el sur del río San Juan al menos hasta esta región de la Precordillera Oriental.
In the eastern fank of the Pedernal hill the Lower Paleozoic stratigraphy is complex and affected by an intense deformation. This paper describes a new section where relicts of Los Azules and Don Braulio formations are recognized for the frst time; these units are overlapping the San Juan Formation and above the La Rinconada For-mation are recorded. This fnding allows extending the paleographic distribution of darriwilian and hirnantian basins southward of the San Juan River at least until this region of the Eastern Precordillera.
Fil: Mestre García, Ana Isabel. Universidad Nacional de San Juan. Facultad de Ingeniería. Instituto de Investigaciones Mineras; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Heredia, Susana Emma. Universidad Nacional de San Juan. Facultad de Ingeniería. Instituto de Investigaciones Mineras; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
https://purl.org/becyt/ford/1.5, ESTRATIGRAFIA, CIENEGUITA, PALEOZOICO, PRECORDILLERA, https://purl.org/becyt/ford/1
https://purl.org/becyt/ford/1.5, ESTRATIGRAFIA, CIENEGUITA, PALEOZOICO, PRECORDILLERA, https://purl.org/becyt/ford/1
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