中文摘要：

Kaigas， Sturtian， Marinoan，和 Gaskiers 冻结成冰广泛地在 Neoproterozoic 被认出。然而，在华南块，仅仅 Jiangkou (Sturtian ) 和 Nantuo (Marinoan ) 被沉积记录象征。Kaigas，由同位素、化学的代理记录了，多半与本地山冻结成冰展出了冷古气候的性质。有 Gaskiers 的 Doushantuo 形成的关联被碳同位素旅行和过时的年龄从间隔显示，然而，华南块当时在非冰川的天气下面。没有 paleomagnetic 数据，华南块的位置不能在 Sturtian 冻结成冰期间是坚定的。华南块的 paleolatitudes 在 Kaigas 和 Nantuo 冻结成冰期间是中间的，尽管 Nantuo 曾经被使变为古怪地推出了赤道。事实上，华南块的 paleolatitudes 都在大约 30 °在 Neoproterozoic 冻结成冰期间是可能的 40 °。

英文摘要：

The Kaigas, Sturtian, Marinoan, and Gaskiers glaciations are widely recognized in Neoproterozoic. However, in the South China Block only the Jiangkou （Sturtian） and Nantuo （Marinoan） are symbolized by sedimentary records. The Kaigas, recorded by isotopic and chemical proxies, exhibited likely the nature of cold paleoclimate with local mountain glaciation. The correlation of the Doushantuo Formation with the Gaskiers is indicated by the carbon isotope excursion and the dated age from the interval, however the South China Block was then under non-glacial weather. With no paleomagnetic data, the position of the South China Block during the Sturtian glaciation cannot be determined. The paleolatitudes of the South China Block during the Kaigas and Nantuo glaciations are intermediate, even though the Nantuo was once rendered erratically deduced equatorial. In fact, the paleolatitudes of the South China Block during the Neoproterozoic glaciations are all likely at about 30°-40°.