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Subduction Zone Magmatism Book

Subduction Zone Magmatism
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Subduction Zone Magmatism, Subduction zones are major sites of volcanism on the Earth. As one crustal plate sinks or is pushed beneath another, hot magma is produced and the resultant magma flux is fundamental to both the thermal evolution and chemical differentiation of the mantle, Subduction Zone Magmatism
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Digital Copy
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  • Subduction Zone Magmatism
  • Written by author Yoshiyuki Tatsumi, Steve Eggins
  • Published by Wiley, John & Sons, Incorporated, 1/1/1995
  • Subduction zones are major sites of volcanism on the Earth. As one crustal plate sinks or is pushed beneath another, hot magma is produced and the resultant magma flux is fundamental to both the thermal evolution and chemical differentiation of the mantle
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Authors

Preface
1 Subduction Zone Magmatism 1
2 Physical Characteristics of Subduction Zone Magmatism 11
3 Geochemical Characteristics of Subduction Zone Magmas 50
4 Hydrous Mineral Stabilities in Subduction Zones: Origin of Dual Volcanic Chains and Across-Arc Geochemical Variation 100
5 Pressure and Temperature of Magma Generation: Origin of Across-Arc Chemical Variation 120
6 Composition of Subduction Zone Fluid Phases: An Experimental Assessment of Geochemical Characteristics 140
7 Mantle Wedge Dynamics 148
References 178
Index 207


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Subduction Zone Magmatism, Subduction zones are major sites of volcanism on the Earth. As one crustal plate sinks or is pushed beneath another, hot magma is produced and the resultant magma flux is fundamental to both the thermal evolution and chemical differentiation of the mantle, Subduction Zone Magmatism

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Subduction Zone Magmatism, Subduction zones are major sites of volcanism on the Earth. As one crustal plate sinks or is pushed beneath another, hot magma is produced and the resultant magma flux is fundamental to both the thermal evolution and chemical differentiation of the mantle, Subduction Zone Magmatism

Subduction Zone Magmatism

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Subduction Zone Magmatism, Subduction zones are major sites of volcanism on the Earth. As one crustal plate sinks or is pushed beneath another, hot magma is produced and the resultant magma flux is fundamental to both the thermal evolution and chemical differentiation of the mantle, Subduction Zone Magmatism

Subduction Zone Magmatism

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