Linking the Wrangellia flood basalts to the Galápagos hotspot
Abstract
The Triassic volcanic rocks of Wrangellia erupted at an equatorial to tropical latitude that was within 3000 km of western North America. The mafic and ultramafic volcanic rocks are compositionally and isotopically similar to those of oceanic plateaux that were generated from a Pacific mantle plume-type source. The thermal conditions, estimated from the primitive rocks, indicate that it was a high temperature regime (TP > 1550 °C) consistent...
Paper Details
Title
Linking the Wrangellia flood basalts to the Galápagos hotspot
Published Date
Apr 21, 2021
Journal
Volume
11
Issue
1
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