31 Stratigraphy (Posters) II
NEW OUTCROPS OF SIERRA GRANDE FORMATION, NORTH PATAGONIAN MASSIF, ARGENTINA
Paper number: 31-28
Program: Technical Sessions
Time: 1:30 PM – 5:30 PM
Authors
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Leonardo StrazzereUniversidad Nacional del Sur, Bahía Blanca, N/A
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Nathalia Migueles Presenting AuthorRadiogenic Isotope Lab, Univ of Wisconsin-Madison, Bahía Blanca, N/A
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Daniel GregoriUniversidad Nacional del Sur y CONICET, Bahía Blanca, N/A
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Vanina LópezUniversidad Nacional del Sur y CONICET, Bahía Blanca, N/A
Abstract
These rocks had been previously mapped as belonging to the Mina Gonzalito Complex, a Proterozoic metamorphic unit that includes gneisses, schists and crystalline calcareous mudstones.
The outcrops constitute a 140 m thick sequence. Three groups with transitional contacts were recognized.
The basal group, 20 m thick, is coarse grain and corresponds to arkoses. Quartz grains are subrounded, equigranular with penetrative contacts. No matrix was recognized. Up to 5% of opaque minerals with ovoidal forms remembering flattened oolites are present.
The middle group (40 m) presents banks 30 to 60 cm thick, with festoon cross-stratification, ripples and antidunes. Channelled forms and point bar migration structures were observed. Paleoflow measuring indicates a NW. (N 310º-340º) provenance.
Toward the superior part of this group, two levels of pure quarzites are recognized.
The upper group (80 m) is conformed by arenites with a coarse, diffuse stratification in banks of 1 m.
The Arroyo Tembrao Stock (Lower Permian) intrusion generated a contact metamorphism evidenced by muscovite and sillimanite (fibrolite) crystallization, conforming a spotted texture.
Textural and compositional characteristics, and also facies arrangement and structures allow us to infer that the basal and middle groups were deposited in a fluvial environment. To the top an increasing of marine influence is observed.
Rocks of similar characteristic were mapped in the Ao. Nahuel Niyeu area, 80 km north-westward. They constitute 500 m of conglomerates, quarzites and arkosic quarzites.
The basal section presents the characteristics of a fluvial environment that passes to a marine environment.
Traditionally it was considered that these rocks were deposited in a marine environment but the new evidence allow us to indicate that some sections would be deposited in a continental environment.