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Figure 5. Pre-Mesozoic geology of the Lambert Glacier drainage basin and Prydz Bay region after Tingey (1982) and Federov (1982). Late Proterozoic metamorphism in the northern Prince Charles Mountains, Mac. Robertson Land, and Ingrid Christensen Coast are mostly granulite facies. The southern Prince Charles Mountains metasediments are generally chlorite grade in some outcrops displaying primary sedimentary structures. Not shown are Mesozoic and Eocene basic igneous dykes in the Beaver Lake area.

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