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《Quaternary Sciences》 2001-03
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THE STRATIGRAPHY AND CHRONOLOGY OF MULTICYCLE QUATERNARY VOLCANIC ROCK-RED SOIL SEQUENCE IN LEIZHOU PENINSULA, SOUTH CHINA

Zhu Zhaoyu, Xu Yifang, Wen Qizhong, Pu Zhiping, Zhou Houyun Wen Gaoguo, Dai Tongmo, Liang Junping, Liang Chisheng, Luo Shuwen (Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640; Bureau of Geology and Mineral Resources of G  
On the basis of a lot of data collected from the field in the Leizhou Peninsula South China,the stratohorizon and the contact relation between the multicycle Quaternary volcanic rock-red soil sequence has been established and their ages have been determinte by using the dating methods, such as U-series isochron dating by total-sample dissolution, Ar-Ar, TL and magnetostratigraphy etc. It is proposed that the sequence can be divided line 7 formations of which ages are 0 - 0.31MaB. P.. 0.31 - 0.48MaB. P. 0.48-0.85MaB. P.. 0.85-1.25MaB. P. l.25- l.65MaB. P. l.652.05MaB.P. and 2.05 - 2.50MaB.P., respectively. There are some types of cycle with different periods, which are 0.057Ma, 0.1Ma, 0.4Ma and 0.8Ma. It indicates there is a similar characteristic in the records of paleo-environmental evolution and global change among the red-soil sequence in South China, the loess-paleosol sequence and the hydrogenic sediment-paleosol sequence in North China, the lake sediment and the glacial till sequence in West China. The formation and evolution of the red soil sequence is probably controlled by the Coupled Climate-Tectonic System following the rule of the Climate-Tectonic Cycle.
【Fund】: 国家自然科学基金(批准号:49772138);; 重大基金(批准号:49894170);; 广东省科学基金(批准号:970562)
【CateGory Index】: P539.2
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