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When Continents Collide Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks

2Gpa has increased to more than 15. This indicates that subduction of continental fragments to depths of 100-150 km may have played a significant role in the formation of mountain belts. This volume brings together the geochemical, geophysical and geodynamical approaches to study the processes active during ultrahigh-pressure (UHP) tectonics. The collection of papers demarkates the frontier of our understanding of the creation, preservation, and exhumation of ultrahigh-pressure rocks. Audience: This volume will be of interest to any earth scientist interested in ultrahigh pressure processes and the formation and modification of continental crust.

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  • "2Gpa has increased to more than 15. This indicates that subduction of continental fragments to depths of 100-150 km may have played a significant role in the formation of mountain belts. This volume brings together the geochemical, geophysical and geodynamical approaches to study the processes active during ultrahigh-pressure (UHP) tectonics. The collection of papers demarkates the frontier of our understanding of the creation, preservation, and exhumation of ultrahigh-pressure rocks. Audience: This volume will be of interest to any earth scientist interested in ultrahigh pressure processes and the formation and modification of continental crust."@en

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  • "Aufsatzsammlung"
  • "Electronic books"@en

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  • "When Continents Collide Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks"@en
  • "When continents collide : geodynamics and geochemistry of ultrahigh-pressure rocks"
  • "When continents collide : geodynamics and geochemistry of ultrahigh-pressure rocks"@en
  • "When Continents Collide: Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks"
  • "When Continents Collide: Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks"@en