Origin And Evolution of the Ontong Java Plateau

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Free Download J G Fitton, J J Mahoney, P J Wallace and A D Saunders, "Origin And Evolution of the Ontong Java Plateau"
English | 2004 | pages: 381 | ISBN: 1862391572 | PDF | 43,9 mb
The Cretaceous submarine Ontong Java Plateau, in the western Pacific Ocean, is the most voluminous of the world's large igneous provinces (LIPs), and represents the largest known magmatic event on Earth. LIPs are the products of basaltic volcanism on a scale and at an effusion rate not seen on Earth at the present time, and their formation may have had significant effects on the Earth's climate and biosphere. The currently favoured explanation for LIP formation is the rapid decompression and melting of anomalously hot mantle in the heads of newly ascended mantle plumes. This volume summarizes the results of research aimed principally at testing the plume-head hypothesis for the formation of the Ontong Java Plateau, and presents the results of integrated studies following recent basement drilling on the plateau by the Ocean Drilling Program.

Nineteen papers cover topics as diverse as petrology, geochemistry, tectonics, volcanology, palaeomagnetism and biostratigraphy.
Also available:
Sumatra: Geology, Resources and Tectonic Evolution (Geological Society Memoirs) - ISBN 1862391807
Tectonics of Strike-Slip Restraining and Releasing Bends - Special Publication no 290 - ISBN 1862392382
The Geological Society of London
Founded in 1807, the Geological Society of London is the oldest geological society in the world, and one of the largest ✅Publishers in the Earth sciences.
The Society publishes a wide range of high-quality peer-reviewed titles for academics and professionals working in the geosciences, and enjoys an enviable international reputation for the quality of its work.
The many areas in which we publish in include:
-Petroleum geology
-Tectonics, structural geology and geodynamics
-Stratigraphy, sedimentology and paleontology
-Volcanology, magmatic studies and geochemistry
-Remote sensing
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