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Detailed studies on Late Devonian to Early Carboniferous carbonate rocks in central Hunan, southern China have led to the recognition of 25 lithofacies which can be grouped into:(1) inner ramp peritidal platform,(2) inner ramp organic bank and mound.(3) mid ramp,(4) outer ramp,and(5) shelf basin fades associations.The peritidal platform fades association dominates the Zimenqiao Formation (Namurian A or late Datangian) and is characterized by gypsum and dolostone-containing sequences, indicating a peritidal platform environment.The other four fades associations dominate the Menggongao Formation(late Famennian).Liujiatang Formation(Tournaisian or Yangruanian).Shidengzi Formations (early Visean or early Datangian).Five upward-shallowing cycles were distinguished in these three Formations.The predominant fades associations developed in each Formation demonstrate an overall transgression-regression cycle in the Late Devonian to Early Carboniferous in central Hunan.The overall transgressive sequence was preserved in the Shaodong.Menggongao.and Liujiatang Formations,and the overall regressive sequence was preserved in the Liujiatang.Shidengzi.Ceshui and Zimenqiao Formations.
Detailed studies on Late Devonian to Early Carboniferous carbonate rocks in central Hunan, southern China have led to the recognition of 25 lithofacies which can be grouped into: (1) inner ramp peritidal platform, (2) inner ramp organic bank and mound. (3 (4) outer ramp, and (5) shelf basin fades associations. The peritidal platform fades association dominates the Zimenqiao Formation (Namurian A or late Datangian) and is characterized by gypsum and dolostone-containing sequences, indicating a peritidal platform environment. the other four fades associations dominate the Menggongao Formation (late Famennian) .Liujiatang Formation (Tournaisian or Yangruanian) .Shidengzi Formations (early Visean or early Datangian) .Five upward-shallowing cycles were distinguished in these three Formations.The predominant fades associations developed in each Formation demonstrate an overall transgression-regression cycle in the Late Devonian to Early Carboniferous in central Hunan. sequence was preserved in the Shaodong. Menggongao. and Liujiatang Formations, and the overall regressive sequence was preserved in the Liujiatang. Hidengzi. Queshui and Zimenqiao Formations.