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Large igneous provinces /
"Large Igneous Provinces (LIPs) are intraplate magmatic events, involving volumes of mainly mafic magma upwards of 100,000 km3, and often above 1 million km3. They are linked to continental break-up, global environmental catastrophes, regional uplift and a variety of ore deposit types. In this...
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| Format: | Printed Book |
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Cambridge
Cambridge University Press
2014
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| Online Access: | http://assets.cambridge.org/97805218/71778/cover/9780521871778.jpg |
Table of Contents:
- Machine generated contents note: Preface; 1. Introduction, definition, and general characteristics; 2. Essential criteria: distinguishing LIP from non-LIP events; 3. Continental flood basalts and volcanic rifted margins; 4. Oceanic LIPs: oceanic plateaus and ocean basin flood basalts and their remnants through time; 5. Plumbing system of LIPs; 6. Archean LIPs; 7. Planetary LIPs; 8. Silicic (Felsic) LIPs; 9. Links with carbonatites, kimberlites, and lamprophyres/lamproites; 10. Geochemistry of LIPs; 11. LIPs and topographic changes; 12. LIPs and rifting; 13. LIPs and links with contractional structures; 14. LIPs and environmental catastrophes; 15. Assessing the origin of LIPs; 16. LIPs and implications for mineral, hydrocarbon and water resources; References; Index.