地球动力学分析表明,古中元古代时,海南岛西部可能经历了一次由“开”向“合”转变的构造演化史。
Geodynamic analysis shows that the tectonic evolution history from "spreading" state into "closing" state might have happened in Paleo Mesoproterozoic age on western Hainan.
本组为评估中元古代生命状况、古环境和前显生宙生物地层提供了重要的生物信息。
This Formation provides important paleobiological information from which to assess status of Mesoproterozoic life, and to evaluate paleoenvironmental conditions and pre_Phanerozoic biostratigraphy.
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