岩石层位学的编译和 geochronological 数据为 Palaeoproterozoic 冰川的忍受 diamictite 继任获得了的这份报纸,并且从而提供卓见进理解引起 Huronian 冻结成冰事件的地质的进程。为这个冻结成冰事件的外观的证据的多数能与 Kenorland supercontinent 决裂有关,对 biogeochemical 的重要大气的变化,以及花蕾联盟氧的光合作用。在这份报纸, Huronian 冻结成冰事件被抑制在 2.292.25 Ga 期间同时地发生了,由包括 pre-2.3 Ga 水圈氧化和 post-2.3 Ga 空气氧化的大氧化事件特征的戏剧的环境变化伴随了。
This paper compiles lithostratigraphic and geochronological data obtained for the Palaeoproterozoic glacial diamictite-bearing successions,and thereby provides insights into understanding the geological processes causing the Huronian Glaciation Event.The majority of evidence for appearances of this glaciation event can be related to the Kenorland supercontinent breakup,allied to significant atmospheric change,as well as blooms of biogeochemical oxygenic photosynthesis.In this paper,the Huronian Glaciation Event is constrained to have occurred synchronously during 2.29-2.25 Ga,accompanied by dramatic environmental changes characteristic of the Great Oxidation Event which includes the pre- 2.3 Ga hydrosphere oxidation and the post-2.3 Ga atmosphere oxygenation.