The Remagnetization of Marine Carbonate Rocks of the Late Ordovician in Pingliang Section,Southwest Ordos(China)
The Remagnetization of Marine Carbonate Rocks of the Late Ordovician in Pingliang Section,Southwest Ordos(China)
摘要
The natural remnant magnetization(NRM)of carbonate rocks in particular must be understood for the construction of a meaningful Paleozoic geomagnetic polarity time scale.This would enable evaluating geomagnetic features(e.g.reversal frequency)and would provide a paleomagnetic dating tool(Voo,1990).
基金
funded by the fundamental research funds for the Central Universities(Grant No.lzujbky-2017-k27)
IGCP652.
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