Inside the Subduction Factory. Volume 138. Geophysical Monograph Series

  • ID: 2489280
  • Book
  • 324 Pages
  • John Wiley and Sons Ltd
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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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Preface vii

Introduction: Inside the Subduction FactoryJohn M. Eiler 1

Section I: The Subducted Slab

Thermal Structure and Metamorphic Evolution of Subducting SlabsSimon M. Peacock 7

Tracers of the SlabTim Elliott 23

Basic Principles of Electromagnetic and Seismological Investigation of Shallow Subduction Zone StructureGeorge Helffrich 47

Section II: The Mantle Wedge

Seismological Constraints on Structure and Flow Patterns Within the Mantle WedgeDouglas A. Wiens and Gideon P. Smith 59

Rheology of the Upper Mantle and the Mantle Wedge: A View From the ExperimentalistsGreg Hirth and David Kohlstedf 83

Experimental Constraints on Melt Generation in the Mantle WedgeGlen A. Gaetani and Timothy L Grove 107

Mapping Water Content in Upper MantleShun–ichiro Karato 135

Section III: Focus Regions

Volcanism and Geochemistry in Central America: Progress and ProblemsM. J. Carr, M. D. Feigenson, L C. Patino, and J. A. Walker 153

n Overview of the Izu–Bonin–Mariana Subduction FactoryRobert J. Stern, Matthew J. Fouch, and Simon L Klemperer 175

Along–strike Variation in Lavas of the Aleutian Island Arc: Genesis of High Mg# Andesite and Implications for Continental CrustPeter B. Kelemen, Gene M. Yogodzinski, and David W. Scholl 223

Section IV: Synthesis

Some Constraints on Arc Magma GenesisYoshiyuki Tatsumi 277

Thermal Structure due to Solid–State Flow in the Mantle Wedge Beneath ArcsPeter B. Kelemen, Jennifer L. Rilling, E. M. Parmentier, Luc Mehl, and Bradley R. Hacker 293

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John Eiler
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