古纬度

按照轴向地心偶极子模型，得出中新世该地区的古纬度为28.3°N。

According to axial geocentre dipole model , the paleolatitude there during Miocene was 28.3 ° N.

改正后的古纬度值能容纳气候带南迁几度的结论，即该地区植被演化是地块北移和冰期来临气候带南迁两种基本因素综合作用的结果。

The corrected value can admit a few degree of southwards migration of climate zone .

其西邻盐源断陷自早三叠世以来南移数百公里，无论古纬度或古方位与东邻地块的结果有较明显差异。

Yanyuan fault-depression has moved southerly about hundreds km since early-Triassic Era , the paleolatitude and paleo-orien-tation were systematically different from those in eastern adjacent block .

本文主要依据三水盆地古地磁数据所反映的华南地块的古纬度漂移讨论南海的演化模式。

In this paper , the authors discuss the evolutionary model of the South China Sea based on the data of Sanshui Basin which indicate the paleolatitude migration of South China .

根据古地磁资料计算得知，罗布泊K1孔的古纬度为34.1°。

Calculation of palaeomagnetic data shows that the palaeolatitude of hole Kl of Lop Nur is 34 . 1 ° N.