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华南海岸上的旧红沙的形成和开发环境在这域和实验室工作里根据调查被讨论。作者相信旧红沙近来是在最后冰川的时期的风神的沉积存款更新世当海水平比礼品低时，并且当海水平相对高时，红土化作用在以后间冰期、冰期后的时期期间发生在热、湿的气候下面。
Formation of 'old red sands' and paleogeographic environment on South China coasts
【摘 要】
：
华南海岸上的旧红沙的形成和开发环境在这域和实验室工作里根据调查被讨论。作者相信旧红沙近来是在最后冰川的时期的风神的沉积存款更新世当海水平比礼品低时，并且当海水平相
【机 构】
：
1.DepartmentofGeography
【出 处】
：
中国科学：地球科学英文版
【发表日期】
：
1998年3期
【基金项目】
：
ProjectsupportedbytheNationalNaturalScienceFoundationofChina (GrantNo .4 96 710 12 ) .
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