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小南屯冰水堆积物的发现
引用本文:程新民.小南屯冰水堆积物的发现[J].吉林地质,1991(2).
作者姓名:程新民
作者单位:长春地质学院
摘    要:小南屯砂砾石层成因争论较大。通过孢粉学研究表明:该孢粉组合是以草本植物花粉为主,木本植物花粉为辅。在草本植物花粉中,又以蒿属占绝对优势,加上藜科、禾本科为特征的干燥寒冷气候带的孢粉组合,表明该砂砾石层为冰水堆积物。

关 键 词:长春郊区  孢粉组合  冰水堆积物  早更新世

DISCOVERY OF GLACIOFLUVIAL SEDIMENT AT XIAONANTUN
Cheng Xinmin.DISCOVERY OF GLACIOFLUVIAL SEDIMENT AT XIAONANTUN[J].Jilin Geology,1991(2).
Authors:Cheng Xinmin
Institution:Changchun College of Geology
Abstract:There are quite different opinions on the origin of sand-gravel beds at Xiaonantun, Jilin. The study of palynology suggests that the pollen of herbage is dominant and that of xylophyta, secondary in the assemblage of spore-pollen. In the herbal plant, Artemisia occupies a absulte dominant position, associated with the pollen assemblage of lamb's-quarters and grass family indicating cold and arid climate. The facts mentioned above indicate that the sand-gravel bed belongs to glaci of luvial deposit.
Keywords:Suburb of Changchun Assemblage of spore-pollen Glaciofluvial deposit Early Pleistocene
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