Citation: | CHEN Fang, SU Xin, D Nurnberg, LU Hong-feng, ZHU You-hua, LIU Jian, LIAO Zhi-liang. LITHOLOGIC FEATURES OF SEDIMENTS CHARACTERIZED BY HIGH SEDIMENTATION RATES SINCE THE LAST GLACIAL MAXIMUM FROM DONGSHA AREA OF THE SOUTH CHINA SEA[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 9-17. |
[1] |
王律江,Sarnthein M.南海北部陆坡近四万年来的高分辨率古海洋记录[J].第四纪研究,1999,19(1):27-31.
[WANG Lü-jiang, Sarnthein M. High-resolution paleoceanographic records since 40 ka ago in the northern continental slope of the South China Sea[J]. Quaternary Researches, 1999,19(1):27-31.]
|
[2] |
Wang P X, Prell W L,Blum P,et al.Proceedings of Ocean Drilling Program, Initial Reports South China Sea[R].V 184,College Station TX(Ocean Drilling Program),1985:18-20.
|
[3] |
汪品先, 卞云华, 王律江, 等. 十五万年来的南海[M]. 上海:同济大学出版社, 1995.[WANG Pin-xian, BIAN Yun-hua, WANG Lü-jiang, et al. The South China Sea Since 150 ka[M]. Shanghai:Tongji University Press, 1995.
]
|
[4] |
冯文科,薛万俊,杨达源,等. 南海北部晚第四纪地质环境[M].广州:广东科技出版社,1988:63-67.[FENG Wen-ke, XUE Wan-jun, YANG Da-yuan, et al. Late Quaternary Geologic Environments in the North of the South China Sea[M]. Guangzhou:Guangdong Science and Technology Press, 1988:63
-67.]
|
[5] |
Martinson D G, Pisias W G, Hays J D, et al. Age dating and the orbital theory of the ice age:development of high resolution 0-300,000 year chronostratigraphy[J]. Quaternary Research,1987,27:1-29.
|