The mafic volcanic climax of the Paraná‐Etendeka Large Igneous Province as the trigger of the Weissert Event-Reference-Cited by-同舟云学术

The mafic volcanic climax of the Paraná‐Etendeka Large Igneous Province as the trigger of the Weissert Event

Published:2021-09-18 Issue:1 Volume:34 Page:28-36
ISSN:0954-4879
Container-title:Terra Nova
language:en
Short-container-title:Terra Nova

Author:

Bacha Rafael R. B.¹,Waichel Breno L.²,Ernst Richard E.¹³

Affiliation:

1. Department of Earth Sciences Carleton University Ottawa ON Canada

2. Departamento de Geociências Universidade Federal de Santa Catarina Florianópolis SC Brazil

3. Faculty of Geology and Geography Tomsk State University Tomsk Russia

Funder

Fundação de Amparo à Pesquisa do Estado de São Paulo

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/ter.12558

Reference34 articles.

1. Contemporaneous alkaline and tholeiitic magmatism in the Ponta Grossa Arch, Paraná-Etendeka Magmatic Province: Constraints from U–Pb zircon/baddeleyite and 40 Ar/ 39 Ar phlogopite dating of the José Fernandes Gabbro and mafic dykes

2. Paraná flood basalt volcanism primarily limited to ~ 1 Myr beginning at 135 Ma: New 40 Ar/ 39 Ar ages for rocks from Rio Grande do Sul, and critical evaluation of published radiometric data

3. Flood Basalt to Rhyolite Suites in the Southern Paran Plateau (Brazil): Palaeomagnetism, Petrogenesis and Geodynamic Implications

4. High‐ and low‐Ti flood basalts from the Paraná plateau (Brazil): Petrogenetic and geochemical aspects bearing on their mantle origin;Bellieni G.;Neues Jahrbuch für Mineralogie ‐ Abhandlungen,1984

5. Giant Circumferential Dyke Swarms: Catalogue and Characteristics

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