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Petrogenesis and stratigraphy of the high-Ti/Y Urubici magma type in the Parana Flood Basalt Province and implications for the nature of 'Dupal'-type mantle in the South Atlantic Region
Journal article   Open access   Peer reviewed

Petrogenesis and stratigraphy of the high-Ti/Y Urubici magma type in the Parana Flood Basalt Province and implications for the nature of 'Dupal'-type mantle in the South Atlantic Region

David W Peate, Chris J Hawkesworth, Nick W Rogers, Simon P Turner and Marta M.S Mantovani
Journal of petrology, Vol.40(3), pp.451-473
1999
DOI: 10.1093/petroj/40.3.451
url
https://doi.org/10.1093/petroj/40.3.451View
Published (Version of record) Open Access

Abstract

The high-Ti/Y Urubici (or Khumib) magma type of the Paraná–Etendeka large igneous province has a restricted spatial extent, near the southeast Brazilian coast and in the northern Etendeka (Namibia). Urubici flows are interbedded with low-Ti/Y Gramado flows. Flow correlations indicate that local topographic relief was important in controlling emplacement of flows, and that lavas near the coast have undergone up to 1 km of post-magmatic uplift relative to inland areas. Urubici magmas have undergone extensive fractional crystallization (MgO <5.5 wt %). Stratigraphic variations highlight complexities of mixing and minor crustal assimilation indicative of open-system magmatic plumbing. The least contaminated samples have high La/Nb (∼1.5) and (Tb/Yb)

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