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Geochemistry of Dominant Low-Ti Basalts of the Siberian Traps and
Subduction-Related Model of Their Origin Ivanov A.V. Institute of the Earth’s Crust, Siberian Branch, Russian Academy of Sciences Flood basalt geochemistry 1.1. Columbia River & Siberian Traps 2. Subduction-related model for flood basalts (Siberian Traps)
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Columbia river Os-isotope data are after Chesley and Ruiz (1998)
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Columbia river Data are plotted after Hooper and Hawkesworth (1993)
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Columbia river Data are plotted after Hooper and Hawkesworth (1993)
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Columbia river
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Columbia river High-Mg basalts of Klyuchevskoi volcano
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Siberian Traps Pangea
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Siberian Traps Ages are for ‘basalts’ only !
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Siberian Traps Approximate size of the Columbia River flood basalts
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Siberian Traps Noril’sk
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Upper Morongovsky subsuite to
Siberian Traps Upper Morongovsky subsuite to Samoedsky suite basalts are not contaminated Saddle Mountains Imnaha Data are plotted after Wooden et al. (1993)
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Siberian Traps Data are plotted after Wooden et al. (1993)
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Siberian Traps
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Siberian Traps
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Siberian Traps Subduction signatures are more prominent
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Model After Ohtani (2005)
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Model Based on Bina et al. (2001), Litasov and Ohtani (2003), Hirschmann et al. (2005)
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Siberian Traps 2300 km Transbaikalian belt (Andean-type orogen)
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Model Transbaikalian belt
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Siberian Traps, Noril’sk event
Model Siberian Traps, Noril’sk event
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Siberian Traps, Tunguska event
Model Siberian Traps, Tunguska event
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Conclusions 1. Primitive mantle-derived flood basalts (with Siberian Traps and Columbia River as examples) show similarities with typical island-arc basalts. They are remarkably different with ocean island basalts. 2. Flood basalt origin can be explained by water-recycling through transition zone of mantle via stagnated (by depth) subduction.
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