仓房沟群冲积体系中钙质结核的成因

1993年 15卷 第1期
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THE ORIGIN OF CALCAREOUS CORES IN THE ALLUVIAL SYSTEM OF THE CANGFANGGOU GROUP
楼章华 赵霞飞
Lou Zhanghua Zhao Xiafei
成都地质学院 610059
Chengdu College of Geology
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。
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.
冲积体系; 钙质结核; 蒸发作用; 气候;
https://doi.org/10.11781/sysydz199301081