Mineralogy, petrology, and origin of the Pedra Branca Suite: a tonalitic-trondhjemitic association with high Zr, Ti and Y, Carajás Province, Amazonian Craton
Open Access
- 1 January 2020
- journal article
- research article
- Published by FapUNIFESP (SciELO) in Brazilian Journal of Geology
Abstract
The Pedra Branca suite (2.75 Ga) is located in the Canaa dos Carajas domain in the southeastern Amazonia Craton. It diverges from typical TTG in mineralogical and geochemical terms, by the presence of hornblende and clinopyroxene and because it has a high content of HFSE (Zr, Y, Ti, and Nb). It belongs to the low-K subalkaline series, which varies from metaluminous to peraluminous, and are mostly calc and ferroan granitoids. Amphibole is calcic and classified as ferroan-edenite, and hastingsite. Plagioclase is mainly oligoclase. The Fe/(Fe + Mg) ratios found in the amphiboles indicate that these granitoids were formed under high to moderate fO(2) conditions. Geobarometric calculations suggest pressures between 9.3 and 71 Kbar for the origin and 4.8-53.4 Kbar for the emplacement. Geothermometric calculations suggest initial crystallization temperatures between 945 and 862 degrees C, and the water content in the magma is estimated to be higher than 4 wt%. The magma source was defined as tholeiitic continental gabbro melted in an extensional setting (Carajas Rift) with geochemical features similar to diabase from Nova Canada (PA). The Pedra Branca magma was originated by partial melting (similar to 28%), leaving a residue with plagioclase (An40), hornblende, clinopyroxene, and may or may not have magnetite.Keywords
This publication has 62 references indexed in Scilit:
- Archean granitoid magmatism in the Canaã dos Carajás area: Implications for crustal evolution of the Carajás province, Amazonian craton, BrazilPrecambrian Research, 2013
- Petrological Constraints on Crystallization Conditions of Mesoarchean Sanukitoid Rocks, Southeastern Amazonian Craton, BrazilJournal of Petrology, 2010
- Secular changes in tonalite-trondhjemite-granodiorite composition as markers of the progressive cooling of EarthGeology, 2002
- 2.8–3.0 Ga plutonism and deformation in the SE Amazonian craton: the Archaean granitoids of Marajoara (Carajás Mineral Province, Brazil)Precambrian Research, 2000
- Th–U–Pb isotopic systems and internal structures of complex zircons from an enderbite from the Pium Complex, Carajás Province, Brazil: evidence for the ages of granulite facies metamorphism and the protolith of the enderbiteChemical Geology, 2000
- Modelling Diverse Processes in the Petrogenesis of a Composite Batholith: the Central Bohemian Pluton, Central European HercynidesJournal of Petrology, 2000
- Crustal evolution in the early Archaean of South America: example of the Sete Voltas Massif, Bahia State, BrazilPrecambrian Research, 1997
- Geochemical changes in baslts and andesites across the Archean-Proterozoic boundary: Identification and significanceLithos, 1989
- Genesis of calc-alkali andesite magma in a hydrous mantle-crust boundary: Petrology of lherzolite xenoliths from the Ichinomegata crater, Oga peninsula, northeast Japan, part IIJournal of Volcanology and Geothermal Research, 1986
- Generation of trondhjemitic-tonalitic liquids and Archean bimodal trondhjemite-basalt suitesGeology, 1976