Structural evolution and significance of a mélange in a collision belt: The Lichi Mélange and the Taiwan arc-continent collision

Keyphrases

• Arc-continent Collision 100%
• Central Range 50%
• Coastal Range 100%
• Collisional Belts 100%
• Deformation Level 50%
• Deformation Zone 50%
• Eurasian Plate 50%
• Flysch Formation 50%
• Forearc Basin 100%
• Geological Map 50%
• Late Miocene 50%
• Lithospheric Subduction 50%
• Longitudinal Valley 100%
• Manila Trench 50%
• Mountain Belts 50%
• Olistostrome 100%
• Ophiolite 50%
• Overriding Plate 50%
• Philippine Sea Plate 50%
• Plate Boundary 50%
• Polygenetic 50%
• Sedimentary Rocks 50%
• Seismic Profiles 50%
• Southeastern Taiwan 50%
• Southern Taiwan 50%
• Structural Evolution 100%
• Structural Profiles 50%
• Structural Significance 100%
• Subduction Complex 100%
• Submarine 100%
• Suture Zone 50%
• Taiwan Arc-continent Collision 100%
• Taiwan Coastal Range 50%
• Tectonic Feature 50%
• Tectonics 50%
• Thrust Fault 50%
• Turbidites 50%
• Weak Zone 50%

Earth and Planetary Sciences

• Arc-Continent Collision 100%
• Eurasian Plate 25%
• Flysch 25%
• Forearc Basin 50%
• Geological Fault 25%
• Miocene 25%
• Olistostrome 50%
• Ophiolite 25%
• Philippine Sea Plate 25%
• Plate Boundary 25%
• Sedimentary Rock 25%
• Structural Evolution 100%
• Taiwan 100%
• Tectonic Feature 25%
• Tectonics 25%
• Trench 25%
• Turbidite 25%