Compactive deformation of incoming calcareous pelagic sediments, northern Hikurangi subduction margin, New Zealand: Implications for subduction processes

Keyphrases

• Pelagic Sediments 100%
• New Zealand 100%
• Subduction Processes 100%
• Slip Rate 66%
• Closely Spaced 33%
• Physical Properties 33%
• Fluid Escape 33%
• Kinematic Modeling 33%
• Tremor 33%
• Normal Fault 33%
• Vertical Profile 33%
• Shear Failure 33%
• Subduction 33%
• Sedimentary Sequence 33%
• Pelagic Carbonates 33%
• Fault Reactivation 33%
• Subduction Zone 33%
• Throwing 33%
• Growth History 33%
• Megathrust 33%
• Syneresis 33%
• Accretionary Wedge 33%
• Paleocene 33%
• Seismic Reflection Data 33%
• Displacement Analysis 33%
• Fault Slip Rate 33%
• Slow Slip Events 33%
• Growth Sequence 33%
• Microearthquakes 33%
• Hikurangi Margin 33%
• Accretion Processes 33%
• Fast Growth 33%
• Lateral Deviation 33%
• Material Heterogeneity 33%
• International Ocean Discovery Program 33%
• Seafloor Deformation 33%
• Rapid Loading 33%
• Fluid Migration 33%
• Pelagic Sedimentation 33%
• Subduction Margin 33%
• Fault Growth 33%
• Drilling Data 33%
• Volumetric Contraction 33%

Earth and Planetary Sciences

• Pelagic Sediment 100%
• New Zealand 100%
• Slip Rate 100%
• Seismic Reflection 33%
• Subduction Zone 33%
• Vertical Profile 33%
• Fault Slip 33%
• Pliocene 33%
• Trench 33%
• Paleocene 33%
• Sedimentary Sequence 33%
• Mudstone 33%
• Accretionary Prism 33%
• Microearthquake 33%
• Growth Fault 33%