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141210s2015 dcu ob 000 0 eng d |
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|a 017073738
|2 Uk
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|a 927509460
|a 929527512
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|a 9781118888995
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|z (OCoLC)927509460
|z (OCoLC)929527512
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|a 9781118888995
|b Wiley
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|a QE511.46 ǂb S833 2016eb
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|a HCDD
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|a Morra, Gabriele,
|e author.
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|a Subduction dynamics /
|c Gabriele Morra.
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|a 1st
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|a Washington, D.C. :
|b American Geophysical Union,
|c 2015.
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|a 1 online resource
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|a text
|b txt
|2 rdacontent
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|a computer
|b c
|2 rdamedia
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|a online resource
|b cr
|2 rdacarrier
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|a Geophysical Monograph Series ;
|v v. 211
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|a CIP data; resource not viewed.
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|a REFERENCES4 Incoming Plate Variations along the Northern Manila Trench: Implications for Seafloor Morphology and Seismicity; 4.1. INTRODUCTION; 4.2. GEOLOGICAL FRAMEWORK; 4.3. INCOMING PLATE VARIATION; 4.4. DISCUSSION; 4.5. CONCLUSION; ACKNOWLEDGMENT; REFERENCES; 5 Source of the Cenozoic Volcanism in Central Asia; 5.1. INTRODUCTION; 5.2. PETROLOGICAL SETTING; 5.3. BUOYANCY DRIVEN VISCOUS INSTABILITIES; 5.4. NUMERICAL SIMULATIONS; 5.5. MODEL RESULTS; 5.6. DISCUSSION; 5.7. CONCLUSIONS; ACKNOWLEDGMENT; BIBLIOGRAPHY; 6 Influence of Variable Thermal Expansivity and Conductivity on Deep Subduction.
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|a Title Page; Table of Contents; CONTRIBUTORS; INTRODUCTION: The Impact of Subduction Dynamics on Mantle Flow, Continental Tectonics, and Seismic Hazard; REFERENCES; 1 Evidence from Caustic Waveform Modeling for Long Slab Thickening above the 660-km Discontinuity under Northeast Asia: Dynamic Implications; 1.1. INTRODUCTION; 1.2. CAUSTIC WAVEFORM MODELING AND DATA SOURCES; 1.3. SLAB IMAGE IN THE MANTLE TRANSITION ZONE; 1.4. UNCERTAINTY ESTIMATES OF THICKNESS OF SLAB; 1.5. DYNAMIC SIMULATION OF SLAB THICKENING; 1.6. DISCUSSION AND DYNAMIC IMPLICATION; 1.7. CONCLUSIONS; ACKNOWLEDGMENT; REFERENCES.
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|a 2 The Continental Collision Process Deduced from the Metamorphic Pattern in the Dabie-Hongseong and Himalayan Collision Belts2.1. INTRODUCTION; 2.2. METAMORPHIC EVOLUTION ALONG THE DABIE-HONGSEONG COLLISION BELT IN NORTHEAST ASIA; 2.3. THE DABIE-SULU COLLISION BELT BETWEEN THE NCB AND SCB IN CHINA; 2.4. THE EXTENSION OF THE DABIE-SULU BELT IN CHINA INTO THE HONGSEONG AREA IN KOREA; 2.5. THE LATE-PERMIAN TO TRIASSIC COLLISION BELT IN KOREA; 2.6. THE EXTENSION OF THE DABIE-HONGSEONG COLLISION BELT INTO JAPAN AND NORTH KOREA; 2.7. THE METAMORPHIC TREND ALONG THE DABIE-HONGSEONG COLLISION BELT.
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|a 2.8. METAMORPHIC EVOLUTION ALONG THE HIMALAYAN COLLISION BELT2.9. THE METAMORPHISM IN THE WESTERN HIMALAYAN COLLISION BELT; 2.10. THE METAMORPHISM IN THE MIDEASTERN HIMALAYAN COLLISION BELT; 2.11. THE METAMORPHISM IN THE EASTERN HIMALAYAN COLLISION BELT; 2.12. THE METAMORPHIC PATTERN ALONG THE HIMALAYA COLLISION BELT; 2.13. DISCUSSION AND TECTONIC IMPLICATION; ACKNOWLEDGMENT; REFERENCES; 3 A New Tectonic Model for the Genesis of Adakitic Arc Magmatism in Cretaceous East Asia; 3.1. INTRODUCTION; 3.2. NUMERICAL MODELSs; 3.3. RESULTS; 3.4. DISCUSSION; 3.5. CONCLUDING REMARKS; ACKNOWLEDGMENT.
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|a 6.1. INTRODUCTION6.2. METHOD AND MODEL; 6.3. RESULTS; 6.4. DISCUSSION AND CONCLUSIONS; ACKNOWLEDGMENT; REFERENCES; 7 Slab-driven Mantle Weakening and Rapid Mantle Flow; 7.1. INTRODUCTION; 7.2. METHODS; 7.3. RESULTS; 7.4. DISCUSSION; 7.5. CONCLUSIONS; ACKNOWLEDGMENT; REFERENCES; 8 Influence on Earthquake Distributions in Slabs from Bimaterial Shear Heating; 8.1. INTRODUCTION; 8.2. NUMERICAL METHOD AND MODEL SETTINGS; 8.3. RESULTS; 8.4. DISCUSSION; 8.5. CONCLUSIONS; ACKNOWLEDGMENT; REFERENCES; 9 The Seismology of the Planet Mongo: The 2015 Ionospheric Seismology Review; 9.1. ORIGINS.
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|a Subduction zones.
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7 |
|a Subduction zones
|2 fast
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| 700 |
1 |
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|a Morra, Gabriele,
|e editor.
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| 700 |
1 |
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|a Yuen, David A.,
|e editor.
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| 700 |
1 |
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|a King, Scott D.,
|e editor.
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| 700 |
1 |
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|a Lee, Sang-Mook,
|e editor.
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| 700 |
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|a Stein, Seth,
|e editor.
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| 776 |
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|i Print version:
|a Morra, Gabriele.
|t Subduction Dynamics: From Mantle Flow to Mega Disasters.
|d : Wiley, ©2015
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| 830 |
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|a Geophysical monograph ;
|v 211.
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4 |
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|u https://ebookcentral.proquest.com/lib/holycrosscollege-ebooks/detail.action?docID=4039563
|y Click for online access
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|a EBC-AC
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|b HCD
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