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The study examines the volcanic rocks of the Cikotok Formation in the Bayah Dome, Banten Province, focusing on their texture, structure, and mineral composition. The findings indicate that these rocks, primarily altered andesite and tuff, originated from shallow eruptions and rapid cooling, characterized by trachytic to porphyritic textures and amygdaloidal structures. The alteration processes are linked to hydrothermal activity and deformation during the Oligo-Miocene period, suggesting these rocks are sig

Author

Muhammad Raihan

Language

EN