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This thesis characterizes Miocene-Pliocene carbonate platforms in the southern Southwest Palawan Basin offshore the Philippines using seismic and well data. The platforms developed on folded and faulted middle Miocene siliclastic strata. They aggraded and backstepped over time to keep pace with rising sea levels. Karst features indicate the platforms were subaerially exposed at times. The platforms terminated in the early Pliocene as sea levels continued rising and they were buried by deep marine siliclasti

Author

Henry Reynolds Darcy

Language

EN