Journal article
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 of petrology, Vol.40(3), pp.451-473
1999
DOI: 10.1093/petroj/40.3.451
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)
Details
- Title: Subtitle
- 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
- Creators
- David W PeateChris J HawkesworthNick W RogersSimon P TurnerMarta M.S Mantovani
- Resource Type
- Journal article
- Publication Details
- Journal of petrology, Vol.40(3), pp.451-473
- DOI
- 10.1093/petroj/40.3.451
- ISSN
- 0022-3530
- eISSN
- 1460-2415
- Language
- English
- Date published
- 1999
- Academic Unit
- Earth and Environmental Sciences; Honors Program
- Record Identifier
- 9983983668302771
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