This hypothesis is only observed oceanic ridges of rock and the residual magnetic field sensors made to return the reverse.
此假说只是观察到岩石和大洋洋脊的感应剩磁场来回反向而提出来的。
These different ophiolite sections actually reflect different dynamic processes beneath oceanic ridges, which are mainly controlled by the plate spreading velocity and the amount of magmatic supply.
不同的蛇绿岩剖面反映了洋脊之下不同的动力学过程，主要受板块扩张速度和岩浆供给的制约。
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