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What is Palaeozoic Geology of Peninsular Malaysia about?

The document summarizes the Palaeozoic sedimentary rocks of Peninsular Malaysia. It divides the area into four stratigraphic zones based on lithology and characteristics: the northwestern zone, western zone, central zone, and eastern zone. Representative lithostratigraphic units are described for each zone. Sedimentation began in the Late Cambrian in the western regime and continued until the Permian. In the eastern regime, sedimentation began in the Early Carboniferous and continued until the Late Permian.

Author

MuhammadHaziqYussof

Language

EN