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Geochemistry and geochronology of the blueschist in the Heilongjiang Complex and its implications in the late Paleozoic tectonics of eastern NE China
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The protolith of the blueschist in the Heilongjiang Complex has an affinity to OIB

The OIB was generated at ~ 280 Ma and subducted after 200 Ma

The OIB represents a big ocean that may be a part of the Paleo-Pacific realm

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