Low- and high-TiO2 flood basalts of southern Brazil: origin from picritic parentage and a common mantle source
- 1 August 1987
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 84 (4) , 423-430
- https://doi.org/10.1016/0012-821x(87)90007-0
Abstract
No abstract availableKeywords
This publication has 23 references indexed in Scilit:
- Evidence from the Parana of south Brazil for a continental contribution to Dupal basaltsNature, 1986
- Trace element and isotopic geochemistry of lavas from Haleakala Volcano, east Maui, Hawaii: Implications for the origin of Hawaiian basaltsJournal of Geophysical Research, 1985
- Petrology of Serra Geral (Paran ) continental flood basalts, southern Brazil: crustal contamination, source material, and South Atlantic magmatismContributions to Mineralogy and Petrology, 1985
- Trace Element and Strontium Isotope Constraints on the Origin and Evolution of Paran Continental Flood Basalts of Santa Catarina State (Southern Brazil)Journal of Petrology, 1985
- Crustal signatures in the Serra Geral flood-basalt province, southern Brazil: O- and Sr-isotope evidenceGeology, 1985
- Flood Basalt to Rhyolite Suites in the Southern Paran Plateau (Brazil): Palaeomagnetism, Petrogenesis and Geodynamic ImplicationsJournal of Petrology, 1984
- A Model for Flood Basalt VulcanismJournal of Petrology, 1980
- Anhydrous melting of peridotite at 0?15 Kb pressure and the genesis of tholeiitic basaltsContributions to Mineralogy and Petrology, 1980
- A variably veined suboceanic upper mantle—Genetic significance for mid-ocean ridge basalts from geochemical evidenceGeology, 1979
- Mesozoic epeirogeny at the South Atlantic margin and the Tristan hot spotGeology, 1976