Rhyacian evolution of subvolcanic and metasedimentary rocks of the southern segment of the Mineiro belt, Sao Francisco Craton, Brazil

Author(s)

Avila, Ciro Alexandre ^[1] ; Teixeira, Wilson ^[2] ; Bongiolo, Everton Marques ^[3] ; Dussin, Ivo Antonio ^[4] ; Teixeira Vieira, Thayla Almeida ^[3]

Affiliation

^[1] Univ Fed Rio de Janeiro, Museu Nacl, Dept Geol & Paleontol, BR-20940040 Rio De Janeiro, RJ - Brazil

^[2] Univ Sao Paulo, Inst Geociencias, BR-05508080 Sao Paulo - Brazil

^[3] Univ Fed Rio de Janeiro, Inst Geociencias, Dept Geol, BR-21949900 Rio De Janeiro, RJ - Brazil

^[4] Univ Sao Paulo, Ctr Pesquisa Geocronol, BR-05508080 Sao Paulo - Brazil

• Document type: Journal article
• Source: Precambrian Research; v. 243, p. 221-251, APR 2014.
• Web of Science Citations: 28

Abstract

The Tiradentes suite in conjunction with the coeval Estacao Tiradentes metasedimentary sequence makes up a distinct tectonic element within the Paleoproterozoic framework of the Mineiro accretionary belt in the Southern Sao Francisco Craton. This suite is the second occurrence of volcanic and subvolcanic rocks in the Mineiro belt and shows petrographic and geochemical similarities with the nearby Serrinha suite (2.23-2.21 Ga) - the first reported Rhyacian volcanism in the Mineiro accretionary belt. The Tiradentes suite is represented by mafic andesites, dacites, granophyres and tonalites and shows petrographic features of volcanic rocks, such as spherulites, amygdales, granophyric intergrowths and porphyritic textures with plagioclase phenocrysts. The rocks of this suite are metaluminous to peraluminous, enriched in alkaline elements, compatible with low-Al2O3 trondhjemites and show primary fractionation of plagioclase, apatite, hornblende, biotite and ilmenite. High HREE content coupled with incipient negative Eu anomaly and high Y values are consistent with a garnet-amphibolite protolith with plagioclase and hornblende as present in the residual phases. The samples of the Tiradentes suite show geochemical signatures of magmatic arcs, which are also observed in rocks from the Serrinha suite. Rocks of the Tiradentes suite yield the following U-Pb zircon crystallization ages: (i) mafic andesite: 2217 +/- 23 Ma; (ii) dacitic dike: 2204 +/- 11 Ma; (iii) subvolcanic tonalite: 2213 +/- 9 Ma. The deposition of the Estacao Tiradentes metasedimentary sequence probably took place after ca. 2088 +/- 12 Ga (although it may be as young as 1990 +/- 39 Ma), according to the U-Pb detrital zircon geochronology of selected samples (diamictite, ferruginous quartzite and carbonaceous phyllite). The Tiradentes rocks show three TOM model ages ranging between 2.4 and 2.3 Ga, indicating short crustal residence for the magmatic protoliths. This inference is also supported by the epsilon(Nd(2.2Ga)) values (+1.1 to +2.3), whereas the respective Sr-87/Sr-86((t)) ratios (0.7018-0.7032) are consistent with the involvement of low Rb/Sr material in the magma genesis, such as a Paleoproterozoic oceanic lithosphere. From a tectonic perspective, the above data are consistent with the idea that a Paleoproterozoic seafloor developed outboard of the Archean-Siderian passive-margin setting (Minas Basin) of the Sao Francisco proto-Craton. The 2.23-2.21 Ga volcanic-subvolcanic rocks of the Tiradentes and Serrinha suites were associated with a Rhyacian oceanic arc. The Estacao Tiradentes metasedimentary sequence (turbidites and distal phyllites) probably formed in back-arc setting concomitant with the Tiradentes suite, as indicated by detrital zircon geochronology. (C) 2014 Elsevier B.V. All rights reserved. (AU)