This study supplies new geological data for research of the early Precambrian crust growth and tectonic evolution of Western Kunlun.

这对研究西昆仑山早前寒武纪陆壳增生及构造演化提供了重要的地质资料。

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This research also reveals that susceptibility can be used as a palaeoclimate proxy for Precambrian successions.

研究结果还表明磁化率能够作为前寒武纪的古气候替代性指标。

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