Neoproterozoic Magmatic Arc Systems of the Central Ribeira Belt, SE-Brazil, in the Context of the West-Gondwana Pre-Collisional History: a Review”
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Journal of South American Earth Sciences xxx (xxxx) xxx Contents lists available at ScienceDirect Journal of South American Earth Sciences journal homepage: www.elsevier.com/locate/jsames Comment to “Neoproterozoic magmatic arc systems of the central Ribeira belt, SE-Brazil, in the context of the West-Gondwana pre-collisional history: A review” Haakon Fossen a,*, Vinicius T. Meira b, Carolina Cavalcante c,d, Jiˇrí Konopasek´ d,e, Vojtecȟ Janouˇsek e a Museum of Natural History/Department of Earth Science, University of Bergen, All´egaten 41, 5007, Bergen, Norway b Instituto de Geoci^encias, Universidade Estadual de Campinas, Campinas, Brazil c Departamento de Geologia, Universidade Federal do Parana,´ Av. Cel. Francisco Heraclito´ dos Santos, 100, Centro Polit´ecnico, Curitiba, PR, 81531-980, Brazil d Department of Geosciences, UiT – The Arctic University of Norway, Dramsveien 201, 9037, Tromsø, Norway e Czech Geological Survey, Klarov´ 3, 118 21, Praha 1, Czech Republic ARTICLE INFO Keywords: Brasiliano orogeny Ribeira belt Intracontinental orogeny 1. Introduction intracontinental orogenic model; 3) the fundamental space problem and failures of the Heilbrons et al.’s (2020) kinematic model; 4) the chro Heilbron et al. (2020) present a review of their model for the Ribeira nology of the orogenic events in the central Ribeira belt that is incom section of the South Atlantic Neoproterozoic orogenic system (SANOS), patible with the timing of multiple terrane collisions implied by which, together with its northward and southward continuation into the Heilbron et al.’s (2020) model, and 5) the geochronologic and strati Araçuaí and Dom Feliciano belts, constitutes the Mantiqueira province graphic constraints from the southern part of the orogenic system, which on the Brazilian side of the South Atlantic Ocean. They lean mainly on is a direct continuation of the Ribeira belt. All these data speak against geochemistry and related tectonic discrimination diagrams as they the presence of a large Adamastor ocean. construct a ~340 m.y. long (860–520 Ma) history of multiple subduc tion, accretion and arc formation events. Their evolutionary history, 2. Geochemical discrimination diagrams must be used with care which has become longer and more complicated over time, has recently been shown to have fundamental problems and is challenged by alter Major- and trace-element based diagrams for discrimination of native interpretations (Meira et al., 2015, 2019a,b; Fossen et al., 2017, geotectonic setting of igneous rocks (e.g., Pearce and Cann, 1973; Pearce 2020; Cavalcante et al., 2019; Konopasek´ et al., 2020). Unfortunately, and Norry, 1979; Pearce et al., 1977; Wood, 1980) have been exten Heilbron et al. (2020) inadequately deal with these problems and sively used (and abused) since they were firstintroduced in early 1970’s. alternative models, thereby missing the opportunity to present an In contrast with the rather grim conclusions of Li et al. (2015), we open-minded and constructive discussion of the orogenic evolution of consider such diagrams as useful projections that may often help to this interesting region. constrain the geodynamic setting of ancient magmatic suites, particu The purpose of this short comment is to expose fundamental prob larly of mafic composition. lems and implications of Heilbron et al.’s (2020) model. We mainly Unfortunately, Heilbron et al. have not chosen a consistent set of comment upon 1) the inconsistent and selective use of geochemical diagrams that would facilitate systematic comparison between individ tectonic discrimination diagrams that makes the authors refuse alter ual magmatic suites discussed in their work. Moreover, several of their native models; 2) their four additional arguments against an diagrams are problematic, and interpreted in a too simplistic way, * Corresponding author. E-mail address: [email protected] (H. Fossen). https://doi.org/10.1016/j.jsames.2020.103052 Received 3 November 2020; Accepted 17 November 2020 Available online 25 November 2020 0895-9811/© 2020 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/4.0/). Please cite this article as: Haakon Fossen, Journal of South American Earth Sciences, https://doi.org/10.1016/j.jsames.2020.103052 H. Fossen et al. Journal of South American Earth Sciences xxx (xxxx) xxx sticking to just one of the possible interpretations and not discussing the 3. Their four arguments against intracontinental orogeny alternatives or simply the entire spread of the data. Nowadays the mostly abandoned diagram of Pearce et al. (1977) (see The first two arguments of Heilbron et al. (2020) that add to the Fig. 7 in Heilbron et al., 2020) is based on the major elements Mg, Fe and purely geochemical argument are the interpretation of some metasedi Al that are fractionated by early magmatic ferromagnesian minerals (e. mentary successions in the Ribeira belt as being fore-arc and back-arc g., olivine, pyroxenes) and feldspars. Hence already the original authors basin deposits, respectively. Since this interpretation is born out of caution against using their MgO–FeOt–Al2O3 plot for intrusive rocks, their own arc model, the argument is circular and will not be dealt with restricting its scope solely to phenocrysts-free lavas. For this reason, this any further. The latter two points concern ultramafic pods (ophiolites) projection seems inappropriate in the present case. and medium to high-pressure metamorphism, and these are treated The diagrams of Pearce et al. (1984), even though still popular in the separately below. granitoid community, also suffer from several shortcomings. In partic ular the Y + Nb vs. Rb diagram, employed also in the current work, 3.1. Mafic pods and ophiolites discriminates (some of the possible) sources of granitic magmas but not necessarily the geodynamic setting of melting. For instance, Well-preserved ophiolites that represent actual oceanic crust are syn-collisional granites are simply assumed to be exclusively strongly typically considered as evidence in support of oceanic subduction. peraluminous, pelite-derived granites, while a variety of other sources However, well-preserved ophiolites have not been found in the Man may be involved, both metasedimentary and metaigneous. Similarly, tiqueira province. Heilbron et al. (2020) mention ultramaficlenses, but Pearce with co-workers stressed that post-collisional granites cannot be their statement that “more complete ophiolitic rock assemblage is pre easily discriminated, as they originate by interaction of magmas coming sent in the Araçuaí belt” is misleading, as those weathered and poorly from variable crustal and mantle sources, depending, among other fac exposed (ultra)mafic metamorphic rocks do not present any ophiolite tors, on the crustal composition of the colliding plates and collision stratigraphy. These ultramaficlenses do not necessarily represent pieces geometry (Pearce, 1996). The ambiguity associated with the discrimi of oceanic crust. They could for example have formed by rift-related nating power of the Y + Nb vs. Rb diagram has been documented by magmatic underplating or hyperextension, and later incorporated into rigorous testing in dedicated work (Forster¨ et al., 1997). the orogen. This is the current interpretation of ultramafic lenses and The high Ba–Sr contents of intermediate to acid magmatic rocks are associated metasediments in the Pyrenees, which is now understood as a taken by Heilbron et al. as evidence for the origin of these from sub modern intracontinental orogenic belt (Clerc et al., 2012; Tugend et al., duction fluid-modified asthenospheric mantle. However, already the 2014). As another example, mafic (metabasalt and metagabbro) and detailed discussion of the Ba–Rb–Sr ternary plot by El Bouseily and El ultramafic rocks of the traditional Alpine ophiolites have been reinter Sokkary (1975) shows that such compositions are characteristic of preted as representing crust/mantle transition at the base of hyper (quartz) diorites, granodiorites and some of the granites. Indeed, one can extended continental crust formed at late stages of rifting (Manatschal propose that similarly low Rb/Ba and Rb/Sr ratios can also be produced et al., 2006; Mohn et al., 2010). Ultramafic lenses also define a certain by partial melting of plagioclase-rich sources, such as metagraywackes tectonostratigraphic level in the Scandinavian Caledonides, interpreted (Sylvester, 1998) or intermediate–basic metaigneous basement (e.g., as exposed subcontinental mantle of hyperextended continental litho Rapp and Watson, 1995). Granulitic, melt-depleted sources stripped of sphere and not oceanic lithosphere, and thus unrelated to the orogenic Rb by some earlier anatectic event represent another viable alternative. suture (Andersen et al., 2012). Hence, ultramafic and mafic rocks in In general, since magmas parental to individual igneous suites in orogenic belts that may appear, and even classify, as ophiolite frag variable geotectonic settings may form from variable sources at a range ments, must not be considered as unambiguous evidence of a of P–T conditions, and further change composition through differenti pre-collisional ocean, let alone oceanic subduction. ation processes such as fractional crystallization/accumulation, magma mixing and/or crustal contamination, geotectonic discrimination dia 3.2. P-T conditions grams do not give absolutely conclusive answers. This was emphasized