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The oxygen, carbon & hydrogen isotope geochemistry of the Phalaborwa Complex, South Africa
The 2060 ± 2 Ma Phalaborwa Complex is a pipe-like ultramafic to carbonatite intrusion formed from multiple magma pulses. This produced a main pipe of pyroxenite, carbonatite and foskorite (olivineapatite-magnetite-calcite) and many smaller syenite plugs around the pipe. The complex is the oldest kno...
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| Language: | English |
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Department of Geological Sciences
2023
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