Language: English
Published on: 1996-01
Hardcover
The Qinglin-Dabie orgogenic belt is a collision zone between the North China and the Yangtze continental blocks. It has a tectonic history of multistage "opening" and "Closing". There are a lot of HP and UHP rocks having been found since the mid of 1980's, and this belt has been a natural laboratory open for international geological research.
Main Contents:
Chapter 1 Introduction;
Chapter 2 Regional geology;
Chapter 3 Geochronology of high-pressure and ultra-high-pressure metamorphic rocks;
Chapter 4 Structural analyses of high-pressure and ultra-high-pressure metamorphic belt;
Chapter 5 Petrology and mineralogy of high-pressure and ultra-high-pressure metamorphic rocks;
Chapter 6 Geochemistry of high-pressure and ultra-high-pressure metamorphic rocks;
Chapter 7 Fluid inclusions in high-pressure and ultra-high-pressure metamorphic rocks;
Chapter 8 PT paths and geodynamics of high-pressure and ultra-high-pressure eclogites;
Chapter 9 Conclusion
