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| PubMed | |
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Article by Zhang, J. W. 1 |
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Article by 2 |
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Article by Wang, X. K. 2 |
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Article by Yuan, X. L. 1 |
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Article by Guo, H. L. 3 |
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Article by Shen, W. X. 3 |
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Article by Chen, Y. 3 |
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Article by Zhou, C. Z. 3 |
Ϊ����̩ɽ�������ļͳ�������������ʯӢɰ�����������������ɼ�̩ɽ���µ��ļͳ�������Ʒ�����۲��о��������ѡW1��W6��6��ʯӢɰ��������ɨ��羵�۲졣��W4�⣬���������������ֳ���̬������Ե������������ж����ı���״�Ͽںͽ���Ƭ��������������ָʾ�ij�������Ϊ��������������������������Ʒ����������Ϊ30.54±2.59 ka B��P����ĩ�α���������ʱ�ξ���ʱ���ϵ��Ǻ��ԡ�
In order to investigate the Quaternary sedimentary environment of Mount Tai��the authors collected Quaternary sediment samples at the south slope of Mount Tai using the analysis method of quartz sand surface characteristics��After laboratory processing��W I-W6 quartz sand particles have been randomly selected to observe under scanning electron microscopy(SEM)��Except W4��other particles showed the characteristics of irregular form�� clear edges��various conehoidal fractures and cleavage fractures��which indicated the glacial deposit environmental condition��Thermoluminescent age of sediment sample was 30.54±2.59 ka B.P., which equaled to the main glacial ice age of the last glaciation��