Volume 13 Issue 5
Sep.  2022
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Guilherme S. Teles, Farid Chemale, Janaína N. Ávila, Trevor R. Ireland. The Paleoarchean Northern Mundo Novo Greenstone Belt, São Francisco Craton: Geochemistry, U-Pb-Hf-O in zircon and pyrite δ34S-Δ33S-Δ36S signatures[J]. Geoscience Frontiers, 2022, 13(5): 101252. doi: 10.1016/j.gsf.2021.101252
Citation: Guilherme S. Teles, Farid Chemale, Janaína N. Ávila, Trevor R. Ireland. The Paleoarchean Northern Mundo Novo Greenstone Belt, São Francisco Craton: Geochemistry, U-Pb-Hf-O in zircon and pyrite δ34S-Δ33S-Δ36S signatures[J]. Geoscience Frontiers, 2022, 13(5): 101252. doi: 10.1016/j.gsf.2021.101252

The Paleoarchean Northern Mundo Novo Greenstone Belt, São Francisco Craton: Geochemistry, U-Pb-Hf-O in zircon and pyrite δ34S-Δ33S-Δ36S signatures

doi: 10.1016/j.gsf.2021.101252

We acknowledge the Brazilian National Council for Scientific and Technological Development (CNPq) for financial support (grants 163459/2013-4 and 202267/2014-8 for G. S Teles and 305053/2014-0 for F. Chemale Jr.), and the Australian Research Council (ARC) (grant DP140103393 for T. R. Ireland). We are thankful to Cid Bonfim for his assistance during fieldwork and to Tiago Girelli for Lu-Hf data acquisition. We would like to thank the Guest Editor Kathryn Cutts and the two anonymous reviewers for valuable comments that helped to improve this paper.

  • Received Date: 2020-10-24
  • Accepted Date: 2021-06-15
  • Rev Recd Date: 2021-06-02
  • Publish Date: 2021-06-17
  • Greenstone belts contain several clues about the evolutionary history of primitive Earth. Here, we describe the volcano-sedimentary rock association exposed along the eastern margin of the Gavião Block, named the Northern Mundo Novo Greenstone Belt (N-MNGB), and present data collected with different techniques, including U-Pb-Hf-O isotopes of zircon and multiple sulfur isotopes (32S, 33S, 34S, and 36S) of pyrite from this supracrustal sequence. A pillowed metabasalt situated in the upper section of the N-MNGB is 3337 ±25 Ma old and has zircon with εHf(t)= -2.47 to -1.40, Hf model ages between 3.75 Ga and 3.82 Ga, and δ18O=+3.6‰ to +7.3‰. These isotopic data, together with compiled whole-rock trace element data, suggest that the mafic metavolcanic rocks formed in a subduction-related setting, likely a back-arc basin juxtaposed to a continental arc. In this context, the magma interacted with older Eoarchean crustal components from the Gavião Block. Detrital zircons from the overlying quartzites of the Jacobina Group are sourced from Paleoarchean rocks, in accordance with previous studies, yielding a maximum depositional age of 3353 ±22 Ma. These detrital zircons have εHf(t)=-5.40 to -0.84, Hf model ages between 3.66 Ga and 4.30 Ga, and δ18O=+4.8‰ to +6.4‰. The pyrite multiple sulfur isotope investigation of the 3.3 Ga supracrustal rocks from the N-MNGB enabled a further understanding of Paleoarchean sulfur cycling. The samples have diverse isotopic compositions that indicate sulfur sourced from distinct reservoirs. Significantly, they preserve the signal of the anoxic Archean atmosphere, expressed by MIF-S signatures (Δ33S between -1.3‰ to +1.4‰) and a Δ36S/Δ33S slope of -0.81 that is indistinguishable from the so-called Archean array. A BIF sample has a magmatic origin of sulfur, as indicated by the limited δ34S range (0 to +2‰), Δ33S~0‰, and Δ36S~0‰. A carbonaceous schist shows positive δ34S (2.1‰-3.5‰) and elevated Δ33S (1.2‰-1.4‰) values, with corresponding negative Δ36S between -1.2‰ to -0.2‰, which resemble the isotopic composition of Archean black shales and suggest a source from the photolytic reduction of elemental sulfur. The pillowed metabasalt displays heterogeneous δ34S, Δ33S, and Δ36S signatures that reflect assimilation of both magmatic sulfur and photolytic sulfate during hydrothermal seafloor alteration. Lastly, pyrite in a massive sulfide lens is isotopically similar to barite of several Paleoarchean deposits worldwide, which might indicate mass dependent sulfur processing from a global and well-mixed sulfate reservoir at this time.
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