[1] LaFond E C. Internal Waves[A] . In: Feirbridge G W,ed. The ency-clopedia of oceanography[C] . New York: Reinhold, 1966. 402~408
[2] Shepard F P, Marshall N F, McLoughlin P A, Sullivan G G. Currentsin submarine canyons and other sea valleys[M] : American Associationof Petroleum Geologists Studies in Geology 8, 1979. 173
[3] Munk W. Internal waves and small - scale processes[A] . In: Warren BA, Wunsch C, eds. Evolution of physical oceanography [C] . Cam-bridge, Massachtsetts Institute of Technology, 1981. 264~191
[4] Gao Zhenzhong, Eri ksson K A. Internal - tide deposits in an Ordovi-cian submarine channel: Previously unrecognized facies? [J] . Geology,1991, 19(7): 734~737
[5] 高振中,Eriksson K A.美国阿巴拉契亚山脉芬卡苏地区奥陶纪海底水道中的内潮汐沉积[J] .沉积学报,1993,11(1):12~22
[6] 高振中,何幼斌,罗顺社,郭建华.深水牵引流沉积-内潮汐、内波和等深流沉积研究[M] .北京:科学出版社,1996
[7] 高振中,何幼斌,李建明,李维峰,罗顺社,王泽中.我国发现内潮汐沉积[J] .科学通报,1997,42(13):1418~1421
[8] 高振中,彭德堂,刘学锋,何幼斌,符翔,李东升,钟广法.塔里木盆地1Z30井中奥陶统内潮汐沉积[J] .江汉石油学院学报,1996,18(4):9~14
[9] Howe J A. Turbidite and contourite sediment waves in the northernRockall Trough, North Atlantic Oeean[J ] . Sedimentology, 1996, 43:219~234
[10] Richard P C, Ritchie J D, Thomson A R. Evolution of deep - waterclimbing dunes in the Rokall Trough - - implications for overflow cur-rents across the Wyville- Thomson Ridge in the Late Miocene[J] .Marine Geology, 1987, 76:177~183
[11] Damuth J E. Migrating sediment waves created by turbidity currentsin the northern south China sea[J] . Geology, 1979, 7:520~523
[12] NorrnarkWR, HessGR, StowDAV, BowenAJ. Sediment waveson the monterey fanlevee: a preliminary physical interpretation[J ] .Marine Geology, 1980, 37:1~18
[13] Flood R D, Sbor A N. Mud waves in the Argentine basin and their re-lationship to regional bottom circulation patterns[J] . Deep - sea Res.,1988, 35:943~971
[14] Gao Zhenzhong, Eriksson K A, He Youbin, et al. Deep- WaterTraction Current Depcsits-A Study of Internal Tides, InternalWaves, Contour Currents and Their Deposits[ M ] . Beijing and NewYork: Science Press, Utrecht and Tokyo: VSP, 1998
[15] Karl H A. Internal - wave currents as a mechanism to account forlarge sand waves in Navarinsky Canyon Head, Bering Sea[J ] . J. Sed-ment. Petrol., 1986, 56(5): 706~714
[16] 张兴阳,高振中,姚雪根.北大西洋洛克尔海槽东北部内波沉积[J] .沉积学报,1999,17(3):464~472
[17] 何幼斌,罗顺社,高振中.深水牵引流沉积研究进展与展望[J] .地球科学进展,1997,12(3):247~252
[18] 何幼斌,高振中.内潮汐、内波沉积的特征与鉴别[J] .科学通报,1998, 43(9): 903~908
[19] Shanmngam G, Spalding T D, Rofheart D H. Process sedimentologyand reservoir quality of deep- marine bottom - current reworked sands(sandy contourites): an example from the Gulf of Mexico[J] . AAPGBulletin,1993,77:1241~1259
[20] 杨殿荣.海洋学[M] .北京:高等教育出版社,1985
[21] LaFond E C. Internal waves[A] . In: Hill M N, ed. The sea[C] Volume 1. London: Wiley Interscience, 1962. 731~751