tectonic rotation

In Cretaceous era, the radius increased and the rotation of the lithosphere plates became slower and drifted to the equator, as Europe and Asia plate drifted relatively to the south opposite to Pacific Ocean plate, forming an extending tectonic style.

进入白垩纪，地球半径增加、岩石圈板块自转减慢且向赤道漂移，由于太平洋板块相对欧亚板块向南漂移，在盆地所在区形成伸展构造样式。

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The method only use inclination data, therefore, the analysis to tectonic rotation is more reliable.

该方法是基于剩磁倾角数据，从而避免了偏角误差的影响，提高了分析的可靠性。

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