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Isotopic composition of two Precambrian stratiform barite deposits from the Indian shield

Journal Article · · Geochimica et Cosmochimica Acta; (USA)
 [1];  [2];  [3]
  1. Delhi Univ. (India)
  2. Geochemisches Institut der Universitaet, Goettingen (West Germany)
  3. Westfalische Wilhelms-Universitaet, Muenster (West Germany)
Stratiform barite beds, interlayered with (fuchsite) quartzites and mafic metavolcanics and containing minor disseminations of sulfides, occur in the Archaean (>3.3 Ga) Sargur Group of rocks at Ghattihosahalli, in the state of Karnataka, south India, and near Jagat, within quartzites and metamorphosed flood basalts underlying the middle Proterozoic ({approximately}2.0 Ga) Aravalli Supergroup in the state of Rajasthan, northwest India. The Sargur barites have {delta}{sup 34}S in the range of 4.02 to 7.45{per thousand}. Disseminations of detrital pyrite, occurring in layers in the barite have {delta}{sup 34}S between {minus}3.62 and {minus}5.87{per thousand}. These barites are also characterized by low {sup 87}Sr/{sup 86}Sr ratios. The basal Aravalli barites, in contrast, have exceptionally high {sup 87}Sr/{sup 86}Sr ratios and {delta}{sup 34}S between 17.11 and 21.4{per thousand}. {delta}{sup 34}S in disseminated chalcopyrite within banded barite-amphibolite samples from the same occurrence varies between 6.21 and 8.52{per thousand}. The isotopic data of the Sargur barites most probably reflect Archean coeval seawater composition. The mantle-like values indicate buffering of the seawater by mantle-derived basaltic crust. In contrast, the Aravalli barites bear the signature of a Proterozoic sea whose sulfur isotope composition is closer to that of present-day oceans. The unusually high {sup 87}Sr/{sup 86}Sr ratios point, however, to a local, highly radiogenic source, which had affected the Sr isotopic composition of coeval, normal seawater.
OSTI ID:
6053502
Journal Information:
Geochimica et Cosmochimica Acta; (USA), Journal Name: Geochimica et Cosmochimica Acta; (USA) Vol. 55:1; ISSN GCACA; ISSN 0016-7037
Country of Publication:
United States
Language:
English

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