THE ORIGIN OF CALCAREOUS CORES IN THE ALLUVIAL SYSTEM OF THE CANGFANGGOU GROUP
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摘要: 冲积体系中的钙质结核是广泛存在的,其成因与沉积环境、沉积速率、气候和排水体系有关。通过分析钙质结核的类型和成因,可以了解冲积体系的古地理特征。Abstract: Calcareous cores are widespread in alluvial systems, and the origin of the cores is related to sedimentary environments, deposition rates, climates and drainage systems. The paleogeographic features of alluvial systems can be recognized by analysing the types and origins of calcareous cores.
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[1] H. H.里丁,周明鉴等译.沉积环境与相.北京:科学出版社.1985.20-80 [2] 赵霞飞.动力沉积学导论与陆相沉积研究,1985 [3] Collison AD, et al. Model and ancient fiuvial system. 1983 [4] Smith RMH. Morphology and depositional history of exhumed Permian point bare in the southwestern Karoo. south Africa. Journal of Sedimentary Petrology, 1987,57(2):19-29 [5] Thomas M,Bown, et al. Integration of channel and floodplain suited.I. Development sequence and lateral relations of alluvial paleosoils. Journal of Sedimentary Petrology, 1987,57(4):587-601
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