Origin of geochemical variability by arc-continent collision in the Biru Area, southern Sulawesi (Indonesia)

Earth and Planetary Sciences

• Magma 100%
• Indonesia 100%
• Arc-Continent Collision 100%
• Trace Element 50%
• Crustal Contamination 50%
• Isotopic Composition 50%
• Volcanic Arc 50%
• Igneous Rock 50%
• Isotopic Ratio 50%
• Mantle Source 50%
• Mid-Ocean Ridge Basalt 50%
• Miocene 50%
• Eocene 50%

Keyphrases

• Microcontinent 100%
• Buton 50%
• Overriding Plate 50%
• Collision Event 50%