Geochemical Correlations among Tholeiitic Plumbing Systems of the South Atlantic-Related Igneous Provinces

45 Pages Posted: 27 Dec 2022

See all articles by Antomat Avelino Macêdo Filho

Antomat Avelino Macêdo Filho

University of Sao Paulo

Maria Helena B.M. Hollanda

University of Sao Paulo

Stephen Fraser

University of Queensland - Sustainable Minerals Institute

Alisson Lopes Oliveira

University of Sao Paulo

Alanny C.C. Melo

University of Queensland - Sustainable Minerals Institute

Alana Régia Dantas

University of Sao Paulo

Date Written: May 24, 2022

Abstract

The opening and spreading of the Atlantic Ocean between Africa and South America evolved during the Early Cretaceous and were preceded by dramatic tholeiitic (mafic) magmatism and minor silicic and alkaline volcanism. These features are presently recognized from the equatorial regions of Brazil and Africa to the Falklands and South Africa. In southeastern South America, continental flood basalts and related plumbing systems constitute the Paraná Magmatic Province (PMP), whose African counterpart is the Etendeka Magmatic Province (EMP). In northeastern Brazil, dike swarms and sill complexes compose the Equatorial Atlantic Magmatic Province (EQUAMP). As a common feature, these provinces are chemically represented by two prevalent magma types: (1) tholeiitic basalts and basaltic andesites with low Ti (TiO2 < 2 wt.%), also including transitional Ti tholeiites with TiO2 ~2.7–1.7 wt.%, and low incompatible element contents. This type is predominantly found in the southern PMP and EMP, with minor occurrences in the EQUAMP. (2) Tholeiitic basalts and basaltic andesites with high Ti (TiO2 > 2 wt.%) and incompatible element contents. High Ti tholeiites are relevant in the northern PMP and EMP, and dominant in EQUAMP. Evolved rocks (SiO2 = 57–65 wt.%) interpreted as byproducts of assimilation and/or fractional crystallization (AFC) processes from high Ti tholeiitic magmas, are scarce (but present) in all three provinces. An accurate analysis of multivariable databases collected from the literature for dikes and sills, including major and trace element and radiogenic isotope data, reveals close similarities in their geochemical signatures. In a paleogeographic reconstruction of West Gondwana, the intrusive remnants of the PMP, EMP and EQUAMP are spread over an area of nearly 10 Mkm², forming perhaps the most extensive set of plumbing systems on Earth, with a relatively consistent chronology based on a vast collection of K–Ar and 40Ar/39Ar data available in the literature. This work provides the first comprehensive data comparison to support the existence of what may have been a single intercontinental-scale magmatic province of West Gondwana.

Keywords: LIP-related plumbing systems, Continental tholeiites, Paraná-Etendeka, EQUAMP, Self-Organizing Maps

Suggested Citation

Macêdo Filho, Antomat Avelino and Hollanda, Maria Helena B.M. and Fraser, Stephen and Oliveira, Alisson Lopes and Melo, Alanny C.C. and Dantas, Alana Régia, Geochemical Correlations among Tholeiitic Plumbing Systems of the South Atlantic-Related Igneous Provinces (May 24, 2022). Available at SSRN: https://ssrn.com/abstract=4289549 or http://dx.doi.org/10.2139/ssrn.4289549

Maria Helena B.M. Hollanda

University of Sao Paulo ( email )

Stephen Fraser

University of Queensland - Sustainable Minerals Institute ( email )

Alisson Lopes Oliveira

University of Sao Paulo ( email )

Alanny C.C. Melo

University of Queensland - Sustainable Minerals Institute

Alana Régia Dantas

University of Sao Paulo ( email )

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