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Magnetic signature of river sediments drained into the southern and eastern part of the South China Sea (Malay Peninsula, Sumatra, Borneo, Luzon and Taiwan)
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文摘
Magnetic fraction in river sediments results from climatic and geological processes. Magnetic fraction dominated in volume by hematite in the southern regions. Magnetic fraction dominated by magnetite/iron sulfide in the northern regions. Potential tracer for paleoclimatic/paleoceanographic changes.

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