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DOI10.1016/j.tecto.2021.228884
Lithosphere of South American intracratonic basins: Electromagnetic and potential field data reveal cratons, terranes, and sutures
Dragone G.N.; Bologna M.S.; Ussami N.; Giménez M.E.; Alvarez O.; Lince Klinger F.G.; Correa-Otto S.
发表日期2021
ISSN00401951
卷号811
英文摘要A magnetotelluric survey comprising 18 broadband stations disposed along a 450 km-long profile was carried out at the transition between the Chaco-Paraná (CPB) and the Paraná (PB) intracratonic basins in northeastern Argentina. Three-dimensional inversions of the responses show that the CPB and southern PB lithospheres are resistive (~103 Ω m) down to 120 km, but with distinct crustal and upper mantle electrical properties. Also, Bouguer gravity and density anomalies are positive at CPB, whereas they are negative at PB. We associate the CPB lithosphere with the Paleoproterozoic Rio Tebicuary craton and the southern PB lithosphere with an ancient and buried piece of craton, the Southern Paraná craton. Geochemical data of mantle xenoliths from the Cenozoic alkaline/carbonatitic province within the Rio Tebicuary craton suggest a subcontinental lithospheric mantle affected by metasomatic processes, which explains its lower resistivity (reaching values as low as 300 Ω m) and higher density (#Mg = 0.87). In contrast, the Southern Paraná craton is more resistive (>103 Ω m) and less dense, suggesting a de-hydrated, depleted, and thicker craton. These cratons are separated by a crustal conductor (15 to 20 km depth; 1–10 Ω m) that we interpret as a southward continuation of a linear anomaly (Paraná Axial Anomaly) defined in former induction studies within the PB in Brazil. Hence, we redefined the trace of this conductive lineament: instead of bending towards the Torres Syncline, it continues inside the CPB. We propose the lineament to be an Early Neoproterozoic suture zone that controlled the location of maximum subsidence in the intracratonic basins during the Paleozoic. In the Early Cretaceous, the Paraná Axial Anomaly was the site of maximum extrusion and deposition of Serra Geral basalts. This anomaly separates compositionally distinct cratonic lithospheres along its path. Melting of this heterogeneous and enriched mantle created the Paraná igneous province. © 2021 Elsevier B.V.
关键词CratonsDensityMagnetotelluricsParanáRio TebicuarySutures
英文关键词Geophysics; Physics; Broadband station; Crustal conductors; Density anomalies; Magnetotelluric surveys; Mantle xenoliths; Metasomatic process; Potential field datum; Sub-continental lithospheric mantles; Structural geology; electrical resistivity; electromagnetic field; igneous province; intracratonic basin; magnetotelluric method; potential field; subsidence; suture zone; upper mantle; Brazil; Parana [Brazil]
语种英语
来源期刊Tectonophysics
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/207965
作者单位Universidade de São Paulo, Instituto de Astronomia, Geofísica e Ciências Atmosféricas, Departamento de Geofísica, São Paulo, Brazil; Instituto Geofísico Sismológico Volponi (IGSV), Universidad Nacional de San Juan, Facultad de Ciencias Exactas, Físicas y Naturales, San Juan, Argentina; Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET), Argentina
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Dragone G.N.,Bologna M.S.,Ussami N.,et al. Lithosphere of South American intracratonic basins: Electromagnetic and potential field data reveal cratons, terranes, and sutures[J],2021,811.
APA Dragone G.N..,Bologna M.S..,Ussami N..,Giménez M.E..,Alvarez O..,...&Correa-Otto S..(2021).Lithosphere of South American intracratonic basins: Electromagnetic and potential field data reveal cratons, terranes, and sutures.Tectonophysics,811.
MLA Dragone G.N.,et al."Lithosphere of South American intracratonic basins: Electromagnetic and potential field data reveal cratons, terranes, and sutures".Tectonophysics 811(2021).
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