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Keyword [Deep Subduction]
Result: 1 - 17 | Page: 1 of 1
1. Geochemistry And Geochronology Of Eclogites From Altyn Tagh And Its Geological Significance
2. Geochemistry Of Deeply Subducted Continental Crust And Fluid Activity During Its Exhumation: Insights From Studies Of The Chinese Continental Scientific Drilling (CCSD) Main-hole Core Samples
3. Metamorphic Dehydration And Partial Melting In Continental Subduction Zones: A Study Of Low-T/UHP Metagranite In South Dabie
4. Experimental Investigation On The Strength Of The Material Near The660Km Discontinuity At High Pressures And Temperatures And Its Implications For Geodynamics
5. Element Geochemical Behavior During The Ultrahigh-pressure Metamorphism
6. Transformation Of Gabbro To Coesite-bearing Eclogite During Deep Subduction In Yangkou Area, North Sulu UHP Terrane
7. Mantle Transition Zone Structures Beneath SE Tibet Revealed By Receiver Functions
8. Ultrahigh-pressure Metamorphism And Partial Melting,and Their Ages In Continental Subduction Zone:Contraints From Granitic Gneisses,Eclogites And Related Amphibolites In The Central Dabie Orogen
9. West Tianshan High-pressure Veins And Host Rocks Typical Mineral Electron Microprobe Analysis And Fluid Tracer Significance
10. Crustal Anatexis During Continental Collision:Evidence From Ultrahigh-pressure Metamorphic Rocks In The Sulu Orogen
11. Nana Er Gold And The Northern Qaidam Victory Mouth Area - UHP Metamorphism Evolution And Melt Flow Activities
12. The Deformation Phases Of Deep Subduction-exhumation Geological Block Of The Yuka Region,the North Qaidam
13. Differential Exhumation And Partial Melting Of HP-UHP Metamorphic Rocks In South Altyn Tagh,NW China
14. Continental Deep Subduction-exhumation Process Of North Qinling Belt:Constraints On Early Paleozoic Tectonic Evolution
15. Partial Melting Of UHP Metamorphic Rocks In The Sulu Orogen And Its Geochemical Effects
16. Detailed Structures Of The 660-km Discontinuity And D" Discontinuity In The Mantle
17. Seismic analysis of the Tonga subduction zone and implications on the thermo-petrologic evolution of deep subduction
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