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Here we report a new study of a gabbroic suite and its associated dioritic and monzogranitic plutons situated in the Yangtze continental interior, the unique continental core in South China, by means of integrated U–Pb dating and Hf isotope analysis of zircon and whole rock Sr–Nd isotope and elemental geochemistry. These intrusive suites are parts of a large batholith (∼970km2) known as the Neoproterozoic...
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