Evidence for Himalayan remagnetization in Tarim Basin
摘要
Himalayan remagnetization in the Tarim Basin was found to be widespread in Paleozoic, Mesozoic and Ce-nozoic rocks. Rock magnetism was performed to study the magnetic carriers. The authors believe that tectonic fluid in the Himalayan stage caused the rock remagnetization. The framboidal pyrites in bitumen and hydrocarbon-rich rocks may transform to framboidal magnetite in the later alkali environment, which leads to remagnetization.
引用本文（GB/T 7714）
Dajun, Fang, Zhongyue, 等. Evidence for Himalayan remagnetization in Tarim Basin[J]. 中国科学通报：英文版, 2002.
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