Mantle deformation in the highly oblique indo-burma subduction system inferred from shear wave splitting measurements

Keyphrases

• Subduction Component 100%
• Mantle Deformation 100%
• Shear Wave Splitting 100%
• Indo-Burma 100%
• Indochina Peninsula 100%
• Sagaing Fault 100%
• Deformational 66%
• Subduction 66%
• Plume 66%
• Burma 66%
• Asthenospheric Flow 66%
• Eastern Indochina 66%
• Fast Polarization Direction 66%
• Indo-Burma Range 66%
• South-East Asia 33%
• Plate Motions 33%
• Subduction Zone 33%
• Subducting Slab 33%
• Upper Mantle 33%
• Dextral 33%
• Anisotropy 33%
• Sudden Transition 33%
• Lag Time 33%
• Late Cenozoic 33%
• Overriding Plate 33%
• Flow Model 33%
• Large-scale Patterns 33%
• Early Cretaceous 33%
• Transform Plate Boundary 33%
• Seismic Network 33%
• Back-arc 33%
• Broadband Seismic 33%
• Low Velocity 33%
• Mantle Flow 33%
• Shallow Mantle 33%
• Teleseismic 33%
• Splitting Analysis 33%
• Null Measurement 33%
• Flow Boundary 33%
• Deformation Fabrics 33%
• Bengal Basin 33%
• Shear-induced 33%
• Indian Plate 33%
• Shan-Thai Block 33%
• Hainan Plume 33%
• Indochina Block 33%
• Subslab 33%
• Kerguelen Plume 33%
• Cenozoic Intraplate Volcanism 33%
• Trench-parallel Flow 33%

Earth and Planetary Sciences

• Myanmar 100%
• Shear-Wave Splitting 100%
• Trench 50%
• Microplate 50%
• Plate Motion 25%
• Volcanism 25%
• Subduction Zone 25%
• Upper Mantle 25%
• Plate Boundary 25%
• Mantle Plume 25%
• Early Cretaceous 25%
• Southeast Asia 25%
• Parallel Flow 25%
• Indian Plate 25%