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Geochemical and Isotopic Signature of a Mesozoic 1000 Km–Long Arcuate Dyke Swarm In NE Brazil
PUBLISHED September 29, 2022 (DOI: https://doi.org/10.54985/peeref.2209p1038798)
NOT PEER REVIEWED
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Authors
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Antomat Avelino Macêdo Filho1 , Maria Helena Hollanda1
- USP
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Conference / event
- 2nd INTERNATIONAL CONGRESS ON EARTH SCIENCES IN SE ASIA, November 2019 (Nusa Dua - Bali, Indonesia)
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Poster summary
- In this work we exposed a preliminary geochemical characterization of the Rio Ceará-Mirim dyke swarm (RCM). This is a giant plumbing system in NE Brazil with ca. 1000 km–long emplaced at the Early Cretaceous age (~130 Ma). The dykes are dominated by high–Ti tholeiites (TiO >2%), followed by low–Ti tholeiites (TiO <2%), rare trachyandesites (SiO >57%) and olivine tholeiites. In this poster we present an integrate characterization of whole–rock geochemistry (major, minor and REE) and Sr–Nd–Pb isotopes of the Rio Ceará–Mirim magmatism.
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Keywords
- Continental tholeiites, Dike swarms, EQUAMP, West Gondwana
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Research areas
- Earth Sciences
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References
- No data provided
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Funding
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- FAPESP (No. 2017/13130–0)
- FAPESP (No. 2017/08423–9)
- FAPESP (No. 2018/24769–5)
- CAPES (No. 1643026)
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Supplemental files
- No data provided
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Additional information
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- Competing interests
- No competing interests were disclosed.
- Data availability statement
- The datasets generated during and / or analyzed during the current study are available from the corresponding author on reasonable request.
- Creative Commons license
- Copyright © 2022 Macêdo Filho et al. This is an open access work distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
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Macêdo Filho, A., Hollanda, M. Geochemical and Isotopic Signature of a Mesozoic 1000 Km–Long Arcuate Dyke Swarm In NE Brazil [not peer reviewed]. Peeref 2022 (poster).
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