The Ordovician and Devonian rocks did not yield reliable character remanence due to either too weak magnetization or dispersal remanent directions.
奥陶系-泥盆系的岩石则由于磁性太弱或方向不稳定，未能获得可靠的特征剩磁方向。
The Ordovician and Devonian rocks did not yield reliable character remanence due to either too weak magnetization or dispersal remanent directions.
奥陶系-泥盆系的岩石则由于磁性太弱或方向不稳定，未能获得可靠的特征剩磁方向。
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