摘要
韩江三角洲ZK37孔第四系中的粘土矿物特征主要由沉积环境控制,它反映了该区的海陆变迁和气侯演化;这些特征与孢粉、微古、指相元素、^(14)C测年等研究结果表明该区晚第四纪存在三个明显的海侵期,而沉积环境变化与古气候有密切联系。
The clay mineral characteristics of the Quaternary sediments of the bore-hole ZK37 in Hanjiang Dalta,controled mainly by the variations of sedimeen-tary environments,reflect a series of interchanges of sea and land and limate of the worked area.The result of clay mineral study,associated with many other investigations such as fossil pollen,foraminiferas,element-indica-tors as well as radiocarbon dates,shows that the deltaic area had three stages of sea transgrassion during the Late Quaternary,The changes of sedimentary environment are relative to the climaic variations.
出处
《中山大学学报（自然科学版）》
CAS
CSCD
1990年第2期133-136,共4页
Acta Scientiarum Naturalium Universitatis Sunyatseni
关键词
韩江三角洲
第四系
古环境
古气候
Hanjiang Delta
clay minerals
palynology
Late Quaternary
paleo-environment
