Stable isotope constraints on vein formation and fluid evolution along a recent thrust fault in the Cascadia accretionary wedge

Keyphrases

• Accretionary Wedge 100%
• Stratigraphy 100%
• Stable Isotopes 100%
• Thrust Fault 100%
• Cascadia 100%
• Vein Formation 100%
• Fluid Pulses 100%
• Fluid Evolution 100%
• Mass Spectrometry Analysis 50%
• Oxygen Isotopes 50%
• In Situ 50%
• Hanging Wall 50%
• Large Earthquake 50%
• Cascadia Margin 50%
• Source Depth 50%
• Secondary Ionization Mass Spectrometry 50%
• General Trends 50%
• Mass Balance 50%
• Ocean Drilling Program 50%
• Thrust Fault System 50%
• Best Explanation 50%
• Crack-seal 50%
• Open Fracture 50%
• Paleoseismicity 50%
• Subduction Margin 50%
• Active Thrust 50%
• Earthquake Events 50%
• Rapid Flow 50%
• Authigenic Calcite 50%
• Accretionary Prism 50%
• Calcite Crystallization 50%
• Calcite Veins 50%
• Structural Balance 50%

Earth and Planetary Sciences

• Geological Fault 100%
• Stable Isotope 100%
• Calcite 100%
• Accretionary Prism 100%
• Stratigraphy 100%
• Footwall 50%
• Ocean Drilling Program 50%
• Mass Spectroscopy 50%
• Paleoseismicity 50%
• Earthquake Event 50%