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The Origin, Evolution, and Environmental Impact of Oceanic Large Igneous Provinces 1-1-001-322-4330-322 The first of four major

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Description

The first of four major deformation events occurred in Jurassic to Early Cretaceous time and is expressed by normal faults recognized in seismic reflection lines and by extensional mylonites in the Tinaquillo alpine-type peridotite

Product Code: SPE524 (Special Paper 524)

Published: 8/20/2008

Published: 9/27/2018

The Origin, Evolution, and Environmental Impact of Oceanic Large Igneous Provinces 1-1-001-322-4330-322 The first of four majorEditors: Clive R. Neal, William W. Sager, Takashi Sano, and Elisabetta Erba The origin, evolution, and environmental impact of large igneous provinces (LIPs) represents a topic of high scientific importance because the magmatism associated with these features cannot be directly related to plate tectonics, and because the eruption of flood basalts may have global environmental consequences. Oceanic LIPs are even more poorly understood due to their

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