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Subduction, Alexander I. Shemenda


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Автор: Alexander I. Shemenda
Название:  Subduction
ISBN: 9789401044110
Издательство: Springer
Классификация:





ISBN-10: 9401044112
Обложка/Формат: Soft cover
Страницы: 217
Вес: 0.36 кг.
Дата издания: 10.10.2012
Серия: Modern Approaches in Geophysics
Язык: English
Издание: Softcover reprint of
Иллюстрации: Xi, 217 p.
Размер: 234 x 156 x 12
Читательская аудитория: Professional & vocational
Основная тема: Geophysics/Geodesy
Подзаголовок: Insights from Physical Modeling
Ссылка на Издательство: Link
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Поставляется из: Германии
Описание: The modeling covers all stages from subduction initiation to `death`, different regimes of subduction producing back arc extension and compression, blocking of subduction and jumps of subduction zone, arc-continent collision and continental subduction.


Inside the Subduction Factory

Автор: Eiler
Название: Inside the Subduction Factory
ISBN: 0875909973 ISBN-13(EAN): 9780875909974
Издательство: Wiley
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Цена: 11238.00 р.
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Описание: Published by the American Geophysical Union as part of the Geophysical Monograph Series, Volume 138.

Subduction zones helped nucleate and grow the continents, they fertilize and lubricate the earth's interior, they are the site of most subaerial volcanism and many major earthquakes, and they yield a large fraction of the earth's precious metals. They are obvious targets for study--almost anything you learn is likely to impact important problems--yet arriving at a general understanding is notoriously difficult: Each subduction zone is distinct, differing in some important aspect from other subduction zones; fundamental aspects of their mechanics and igneous processes differ from those in other, relatively well-understood parts of the earth; and there are few direct samples of some of their most important metamorphic and metasomatic processes. As a result, even first-order features of subduction zones have generated conflict and apparent paradox. A central question about convergent margins, for instance--how vigorous magmatism can occur where plates sink and the mantle cools--has a host of mutually inconsistent answers: Early suggestions that magmatism resulted from melting subducted crust have been emphatically disproved and recently just as emphatically revived; the idea that melting is fluxed by fluid released from subducted crust is widely held but cannot explain the temperatures and volatile contents of many arc magmas; generations of kinematic and dynamic models have told us the mantle sinks at convergent margins, yet strong evidence suggests that melting there is often driven by upwelling. In contrast, our understanding ofwhy volcanoes appear at ocean ridges and "hotspots"--although still presenting their own chestnuts--are fundamentally solved problems.


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