When Continents Collide: Geodynamics and Geochemistry of Ultrahigh-Pressure Rocks

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Bradley Hacker, J.G. Liou
Springer Science & Business Media, 11.11.2013 - 325 Seiten
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.
 

Inhalt

Table of Contents
Implications for Geodynamics
References
Melting of Crustal Rocks During Continental Collision
Melting Phase Relations of Common Crustal Rocks
Rheology of Crustal Rocks at Ultrahigh Pressure
Discussion
Thermal Controls on Slab Breakoff and the Rise
Introduction 2 Background
Plate Rates
Exhumation Rates
Surface Uplift
Effects of Climate
Mechanisms of Erosion
Conclusions
KAr 40Ar39Ar Geochronology of Ultrahigh

Applications to Collisional Orogens
Conclusions
Thermal Boundary Conditions and Cooling History
Introduction
Temperature History During Exhumation of UHP Rocks
Modeling of Exhumation
Exhumation Rates and Cooling Rates in UHP Rocks
Application of the Modeling to the QinlingDabie Orogenic Belt Central China
Conclusions
Acknowledgments References
Appendix
Active Tectonics and UltrahighPressure Rocks
Fluid Recycling FluidRock Interactions and the arisotopic
Conclusions
Geochemical and Isotopic Characteristics of
Introduction
Notation
Conclusions
Discussion
Phase
Discussion
Field Examples of Incomplete Eclogitization
The Role of Deformation and Fluid in Metamorphism of
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