Early Carboniferous paleomagnetic results from the northeastern margin of the Qinghai-Tibetan plateau and their implications
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文摘

A paleomagnetic work was carried out in the Carboniferous strata in Qaidam Basin.

The characteristic remanent magnetization passed fold test.

Our results indicated a paleolatitude of 13.5°N for the Qaidam block.

The Qaidam block was independent from North China, South China and Tarim Block.

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