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Title: Geochemical indicators of provenance and tectonic setting of Mississippian pelites of the Ouachita fold belt

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:5591356
 [1]; ;  [2]
  1. Univ. of New Orleans, LA (United States)
  2. Univ. of Oklahoma, Norman, OK (United States)

Plate tectonic reconstructions of the southern continental margin of North America during the Paleozoic are inconclusive. Numerous conflicting models have been proposed for the opening and closing of the Iapetus Ocean and the subsequent deposition and deformation of the Ouachita System. Considerable confusion also exists concerning the provenance of the Carboniferous flysch deposits of the Ouachitas. Trace element geochemistry of shales from the Stanley Group constrain both the provenance of the sediments and the plate tectonic setting during the Mississippian evolution of the southern continental margin. Th/Sc and Cr/Th ratios support a cratonic source for the majority of samples analyzed. However, in several samples the Th/Sc ratio decreases and the Cr/Th ratio increases, suggesting a contribution from a more mafic source. Using element ratio-ratio diagrams, all of the samples plot along a curve consistent with a two-component mixing model between a felsic and a mafic source. Both a tantalum-niobium trough and a strongly negative strontium anomaly are seen in upper-crust-normalized trace element spiderdiagrams. These anomalies are also present in interbedded volcaniclastics within the Stanley. The Stanley shales also exhibit a positive vanadium-chromium-nickel anomaly. The pervasive occurrence of these anomalies is interpreted as inherited from their source, and not from diagenetic alteration or sedimentary processes.

OSTI ID:
5591356
Report Number(s):
CONF-921058-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 24:7; Conference: 1992 annual meeting of the Geological Society of America (GSA), Cincinnati, OH (United States), 26-29 Oct 1992; ISSN 0016-7592
Country of Publication:
United States
Language:
English