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An intensive paleomagnetic investigation has been conducted on the Middle Triassic Leikoupo Formation on the Wangcang section (32.14°N, 103.17°E). The results indicate the magnetic minerals are dominant by multi domain magnetite or maghemite, and the characteristic remnant magnetization revealed by stepwise thermal/alternating field demagnetization is close to the present day geomagnetic direction of the sampling site. This suggests that dolomitization/thermal viscous magnetization is responsible for the remagnetization of this kind of rocks.
An intensive paleomagnetic investigation has been conducted on the Middle Triassic Leikoupo Formation on the Wangcang section (32.14 ° N, 103.17 ° E). The results indicate the magnetic minerals are dominant by multi domain magnetite or maghemite, and the characteristic remnant magnetization revealed by stepwise thermal / alternating field demagnetization is close to the present day geomagnetic direction of the sampling site. This suggests that dolomitization / thermal viscous magnetization is responsible for the remagnetization of this kind of rocks.