Magnetic signature of river sediments drained into the southern and eastern part of the South China Sea (Malay Peninsula, Sumatra, Borneo, Luzon and Taiwan)
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.