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140122 ||| eng |
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|a 9783642680120
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| 100 |
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|a Gill, J. B.
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| 245 |
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|a Orogenic Andesites and Plate Tectonics
|h Elektronische Ressource
|c by J. B. Gill
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| 250 |
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|a 1st ed. 1981
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| 260 |
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|a Berlin, Heidelberg
|b Springer Berlin Heidelberg
|c 1981, 1981
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| 300 |
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|a XIV, 392 p
|b online resource
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| 505 |
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|a 1 What is “Typical Calcalkaline Andesite”? -- 1.1 Introduction -- 1.2 Definition of Orogenic Andesite -- 1.3 Magma Series Containing Orogenic Andesites -- 1.4 Overview -- 2 The Plate Tectonic Connection -- 2.1 Spatial Distribution of Active Orogenic Andesite Volcanoes -- 2.2 Initiation of Subduction -- 2.3 Cessation of Subduction -- 2.4 Collisions -- 2.5 Reversal of Subduction Polarity -- 2.6 Forearc and Transform Fault Volcanism -- 2.7 Anomalously Wide Volcanic Arcs -- 2.8 Andesites Clearly Not at Convergent Plate Boundaries -- 2.9 Conclusions -- 3 Geophysical Setting of Volcanism at Convergent Plate Boundaries -- 3.1 Topography, Gravity, Heat Flow, and Conductivity -- 3.2 Crustal Thickness, Structure, and Age -- 3.3 Upper Mantle Beneath the Forearc, Volcanic Arc, and Backarc Regions -- 3.4 Dipping Seismic Zones (Benioff-Wadati Zones) and Underthrust Lithosphere -- 3.5 Partial Melting and Magma Ascent Beneath Volcanic Arcs --
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|a 8.1 Characteristics of Subducted Ocean Crust Beneath Volcanic Arcs -- 8.2 Circumstantial Evidence of Slab Recycling in Arc Volcanism -- 8.3 Are Orogenic Andesites Primary Melts of Subducted Ocean Floor Basalt? No -- 8.4 The Sediment Solution -- 8.5 IRS Fluids and Maxwell’s Demons -- 8.6 Conclusions -- 9 The Role of the Mantle Wedge -- 9.1 Characteristics of the Mantle Wedge -- 9.2 Circumstantial Evidence that Arc Magmas Originate Within the Mantle Wedge -- 9.3 Are Orogenic Andesites Primary Melts of Only the Mantle Wedge? Rarely -- 9.4 Fluid Mixing, Metasomatism, and Demonology in the Mantle Wedge -- 10 The Role of the Crust -- 10.1 Circumstantial Evidence for Crustal Involvement in Orogenic Andesites -- 10.2 Crustal Anatexis -- 10.3 Crustal Assimilation -- 11 The Role of BasaltDifferentiation -- 11.1 General Arguments for and Against Differentiation -- 11.2 Roles of Plagioclase, Pyroxenes, and Olivine --
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|a 5.7 Geochemical Distinctiveness of Volcanism at Convergent Plate Boundaries -- 5.8 Conclusions: Chemical Diversity of Orogenic Andesites -- 6 Mineralogy and Mineral Stabilities -- 6.1 Plagioclase -- 6.2 Pyroxenes -- 6.3 Amphibole -- 6.4 Olivine -- 6.5 Oxides -- 6.6 Garnet -- 6.7 Other Minerals -- 6.8 Inclusions in Orogenic Andesites -- 6.9 Mineral Stabilities in Andesite Magma -- 6.10 Trace Element Equilibria Between Minerals and Melt -- 6.11 Conclusions -- 7 Spatial and Temporal Variations in the Composition of Orogenic Andesites -- 7.1 Variations in Magma Composition Across Volcanic Arcs -- 7.2 Variations in Magma Composition Along Volcanic Arcs -- 7.3 Effects of Plate Convergence Rate on Magma Composition -- 7.4 Relationships Between Compositions of Orogenic Andesites and Adjacent Oceanic Crust -- 7.5 Changes in the Composition of Orogenic Andesites During Earth History -- 8 The Role of Subducted Ocean Crust in the Genesis of Orogenic Andesites --
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|a 3.6 Magma Chambers Beneath Orogenic Andesite Volcanoes -- 3.7 Conclusions -- 4 Andesite Magmas, Ejecta, Eruptions, and Volcanoes -- 4.1 Characteristics of Andesite Magma -- 4.2 Andesite Rock, Eruption, and Edifice Types -- 4.3 Variations in Magma Composition During and etween Historic Andesite Eruptions -- 4.4 Variations in Rock Composition During Evolution of Stratovolcanoes -- 4.5 Conclusions About Andesite Magma Reservoirs -- 4.6 Stress Fields and Volcano Spacings Within Volcanic Arcs -- 4.7 Relationships Between the Timing of Arc Volcanism and Plate Movements -- 4.8 Magma Eruption Rates at Convergent Plate Boundaries -- 4.9 Relative Proportions of Andesite -- 5 Bulk Chemical Composition of Orogenic Andesites -- 5.1 Rock Analyses: Significance, Averages, and Representative Samples and Suites -- 5.2 Major Elements -- 5.3 Volatiles -- 5.4 Trace Elements -- 5.5 Isotopes -- 5.6Comparison with Andesites Not at Convergent Plate Boundaries --
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|a 11.3 Role of Magnetite and the Plagioclase-Orthopyroxene/Olivine-Augite-Magnetite (POAM) Model -- 11.4 Role of Amphibole -- 11.5 Role of Garnet -- 11.6 Role of Accessory Minerals: Apatite, Chromite, Sulfides, Biotite -- 11.7 Role of Magma Mixing -- 11.8 Role of Other Differentiation Mechanisms -- 11.9 Differentiation Processes Leading to Andesites in Anorogenic Environments -- 12 Conclusions -- 12.1 Andesite Genesis by POAM-Fractionation: the Most Frequent Mechanism -- 12.2 Some Outstanding Problems Requiring Clarification -- 12.3 Origin of Tholeiitic Versus Calcalkaline Andesites -- 12.4 Origin of Across-Arc Geochemical Variations -- 12.5 Epilog -- References
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| 653 |
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|a Geology
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| 653 |
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|a Mineralogy
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| 041 |
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7 |
|a eng
|2 ISO 639-2
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| 989 |
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|b SBA
|a Springer Book Archives -2004
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| 490 |
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|a Minerals, Rocks and Mountains
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| 028 |
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|a 10.1007/978-3-642-68012-0
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| 856 |
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|u https://doi.org/10.1007/978-3-642-68012-0?nosfx=y
|x Verlag
|3 Volltext
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|a 549
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| 520 |
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|a Students of a phenomenon as common but complex as andesite genesis often are overwhelmed by, or overlook, the volume and diversity of relevant information. Thus there is need for periodic overview even in the absence of a dramatic breakthrough which "solves the andesite problem" and even though new ideas and data keep the issues in a state of flux. Thus I have summarized the subject through mid·1980 from my perspective to help clarify the long-standing problem and to identify profitable areas for future research. Overviews are more easily justified than achieved and there are fundamental differences of opinion concerning how to go about them. It is professionally dangerous and therefore uncom mon for single authors, especially those under 35 such as I, to summarize a broad, active field of science in book-length thor oughness. Review articles in journals, multi-authored books, or symposia proceedings appear instead. The single-authored approach is intimidating in scale and can result in loss of thoroughness or authority on individual topics. The alternatives lack scope or integration or both
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