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对大西洋、太平洋、印度洋、北极等海域,已经建立了第三纪和白垩纪大洋岩石圈的板块构造模式。但是,由于海盆过于年轻,并且不断被消减带所吞噬,人们无法把磁化条带得出的这些模式推广到白垩—侏罗纪以前。为了进一步建立中生代和古生代的模式,必须依靠大陆地壳的资料,然而仅凭单一的地质证据一般不能得到岩石圈板块分布的最好答案。但是,如果能确定板块随时间变化的特性并弄清
For the Atlantic, Pacific, Indian Ocean, Arctic and other sea areas, Tertiary and Cretaceous oceanic lithospheric plate tectonics have been established. However, because the basin is too young and is constantly being swallowed up by the abatement zone, one can not generalize the patterns derived from magnetized bands to the Cretaceous-Jurassic. In order to further establish the Mesozoic and Paleozoic models, the data of the continental crust must be relied upon. However, the best answer to the lithospheric plate distribution can not generally be obtained by a single geological evidence. However, if one can determine the nature of the plate over time and figure it out