[1] Stuut J-B W, Prins M A, Schneider R R, et al. A 300-ka record of aridity and wind strength in southwestern Africa: inferences from grain-size distribution of sediments on Walvis Ridge, SE Atlantic[J]. Marine Geology, 2002, 180: 221～233
[2] Prins M A, Postma G, Weltje G J. Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Makran continental slope[J]. Marine Geology, 2000, 169: 351～371
[3] Gingle F X, Schmieder F, Dobeneck T, Petschick, et al. Terrigenous flux in the Rio Grande Rise area during the past 1500 ka: Evidence of deepwater advection or rapid response to continental rainfall patterns?[J]. Paleoceanography, 1999, 14(1): 84～95
[4] 秦蕴珊等. 东海地质[M]. 北京:科学出版社,1987 [ Qin Y S, et al. Geology of East China Sea[M]. Beijing: Science Press, 1987]
[5] 潘志良,石斯器. 冲绳海槽沉积物及其沉积作用的研究[J]. 海洋地质与第四纪地质. 1986,6(1):17～29 [Pan Z L, Si S Q. Study on sediments and sedimentation in Okinawa Trough[J]. Marine Geology and Quaternary Geology, 1986,6: 17～29]
[6] 郑铁民,徐善民,徐志明. 冲绳海槽表层沉积物沉积特征的初步研究[J]. 海洋与湖沼. 1986, 20(2): 113～121[Zheng T M, Xu S M, Xu Z M. Characteristics of the surface sediments in Okinawa Trough[J].Oceanologia et Limnologia Acta,1986,20(2):113～121]
[7] 张明书. 冲绳海槽沉积物分类和层序划分的初步意见[J]. 海洋地质与第四纪地质. 1986, 6(2):31～40[ Zhang M.S. The preliminary suggestion to the sediment classification and strata sequence in Okinawa Trough[J]. Marine Geology and Quaternary Geology, 1986,6 (2):31～40]
[8] 袁迎如,陈冠球,杨文达等. 冲绳海槽沉积物的特征[J]. 海洋学报. 1987, 9(3): 353～360 [Yuan Y R, Chen G Q, Yang WD, et al. The characteristics of Sediments in Okinawa Trough[J]. Acta Oceanologica Sinica, 1987, 9(3): 353～360]
[9] 袁迎如. 冲绳海槽沉积物的粒度[J]. 东海海洋,1987, 4(3):, 42～49[Yuan Y.R. Grain-size of the sediments in Okinawa Tough[J]. Donghai Marine Science, 1987, 4(3): 42～49]
[10] Katayama H. Transport processes of terrigenous materials to the Okinawa Trough based on chemical and mineralogical analysis of settling particles [A]. In: Hu D, Tsunogai S, eds. Margin flux in the East China Sea[C]. Beijing: China Ocean Press, 1999. 42～48
[11] Hu D X. The role of vertical circulation in sediment dynamics[A]. In: Ye D Z, Lin H, eds. China Contribution to Global Changes Studies [C]. Beijing: China Science Press, 1995.168～170
[12] Yanagi T S, Takahashi and Hoshika A. Seasonal variation in the transport of suspended matter in the East China Sea [J]. Journal of Oceanography, 1996, 52:539～552
[13] Peng M C, Hu D X. Outflow of suspended materials from Changjiang River Mouth [J].Chin. J. Oceanol. Limnol., 1997,15:258～263
[14] Rea D K, Janecek T R. Mass accumulation rates of the non-authigenic inorganic crystalline (eolian) components from the western Mid-Pacific Mountains [A].In: Thiede, et al, eds. Deep Sea Drilling Project Site 463, Initial Report of Deep Sea Drill Project [R]. 1981, 62: 653～659
[15] 孙有斌,高抒,鹿化煜. 前处理方法对北黄海沉积物粒度的影响[J]. 海洋与湖沼, 2001, 32(6): 665～671[ Sun Y B, Gao S, Lu H Y. Influence of different pretreatment procedures on the particle-size distribution of surfacial sediments in the Northern Yellow Sea.[J]. Oceanologica et Limnologica Sinica, 2001, 32(6): 665～671]
[16] 鹿化煜, 苗晓东, 孙有斌. 前处理步骤与方法对风成红粘土粒度测量的影响[J].海洋地质与第四纪地质,2002, 22(3): 129～135[Lu H Y, Miao X D, Sun Y B. Pretreatment methods and their influences on grain-size measurement of aeolian "Red Clay" in North China[J]. Marine Geology and Quaternary Geology, 2002, 22(3): 129～135]
[17] 苏纪兰,秦蕴珊. 当代海洋科学学科前沿 [C]. 北京:学苑出版社, 2000. 190～191[Su J L, Qin Y S. Frontiers of contemporary marine science[C]. Beijing: Xueyuan Press, 2000. 190～191]
[18] 金性春等. 大洋钻探与中国地球科学[M]. 上海:同济大学出版社, 1995 [Jin X C, et al. Ocean drilling program and earth sciences in China [M]. Shanghai: Tongji University Press, 1995]
[19] 高抒,贾建军. 冲绳海槽中北部及邻近陆坡近表层物质的粒度特征[A]. 见:高抒,李家彪主编. 中国边缘海的形成演化[C]. 北京:海洋出版社,2002. 125～139 [ Gao S, Jia J J. The grain-size charatercistics of the near surface sediment in the Mid-North Okinawa Trough and its vicinities[A]. In: Gao S, Li J B, eds. The formation and evolution of Chinese Marginal Seas[C]. Beijing: Ocean Press, 2002. 125～139]
[20] 蒋富清,李安春, 李铁钢. 冲绳海槽南部柱状沉积地球化学特征和古环境意义[J].海洋地质与第四纪地质, 2002, 22(3): 11～17[Jiang F Q, Li A C, Li T G. Geochemical characteristics for core sediments of the southern Okinawa Trough and its paleoclimatic implication[J]. Marine Geology and Quaternary Geology, 2002, 22(3): 11～17]
[21] Sibuet J C, Deffontaines B, Hsu S K, Thareau N, Le Formal, et al. Okinawa Trough backarc basin: early tectonic and magmatic evolution[J]. Journal of Geophysical Research, 1998, 103: 30245～30267
[22] 李巍然,杨作升,王琦等. 冲绳海槽陆源碎屑峡谷通道搬运与海底扇沉积[J]. 海洋与湖沼, 2001,32(4): 371～380 [ Li W Z., Yang Z S, Wang Q, et al. Terrigenous transportation through canyon and sedimentation of submarine fan in the Okinawa Trough[J]. Oceanologia et Limnologia Acta, 2001,32(4):371～380]
[23] 谢钦春, 叶银灿, 陆炳文. 东海陆架坡折地形和沉积作用过程[J]. 海洋学报, 1984, 6: 61～71 [Xie Q C, Ye Y C, Lu B W. The topography of slop break in the East China Sea Shelf and sedimentation process [J]. Acta Oceanica Sinica, 1984, 6: 61～71]
[24] Salaheldin T M, Imran J, Chaudhry M H, Reed C. Role of fine-grained sediment in turbidity current flow dynamics and resulting deposits[J]. Marine Geology, 2000, 171: 21～38
[25] Chung Y C, Hung G W. Particulate fluxes and transports on the slope between the southern East China Sea and the South Okinawa Trough [J]. Continental Shelf Research, 2000, 20: 571～597
[26] Yanagi T, Morimoto A, Ichikawa K. Seasonal variation in surface circulation of the East China Sea and the Yellow Sea derived from satellite altimetric data [J]. Continental Shelf Research, 1997,17(6):655～664
[27] Salibury M H, Shinohara M, Richter C, et al. Shipboard Scientific Party Chapter 5, Site 1202, in Proceeding of the Ocean Drilling program, Initial Reports[R]. 2002.195