[1]Heezen B C, Ewing W M. Turbidity currents and submarine slumps and the 1929 Grand Banks (Newfoundland) earthquake[J]. American Journal Science Series,1952,250:849-873.
[2]Parker G, Garcia M, Fukushima Y, et al. Experiments on turbidity currents over an erodible bed[J].Journal of Hydraulic Research,1987,25:123-147, doi: 10.1080/00221688709499292.
[3]Garcia M. Depositional turbidity currents laden with poorly sorted sediment[J].Journal of Hydraulic Engineering,1994,120:1 240-1 263, doi: 10.1061/ASCE0733-9429(1994)120:11(1240).
[4]Huang H, Imran J, Pirmez C. Numerical modeling of poorly sorted depositional turbidity currents[J].Journal of Geophysical Research,2007,112: 1-15.
[5]Bouma A H, Normark W R, Barnes N E. Submarine Fans and Related Turbidite Systems[M].New York:Springer Verlag, 1985: 351.
[6]Talling P J, Masson D G, Sumner E J, et al. Subaqueous sediment density flows: Depositional processes and deposit types[J].Sedimentology, 2012,59(7): 1 937-2 003, doi:10.1111/j.1365-3091.2012.01353.x.
[7]Hsu S K, Kuo J, Lo C L, et al. Turbidity currents, submarine landslides and the 2006 Pingtung earthquake off SW Taiwan[J].Terrestrial, Atmospheric and Oceanic Science, 2008, 19:767-772, doi:10.3319/TAO.2008.19.6.767(PT).
[8]Inman D L, Nordstrom C E, Reinhard E F. Currents in submarine canyons: An air-sea-land interaction[J].Annual Review of Fluid Mechanics,1976, 8:275-310, doi: 10.1146/annurev.fl .08.010176.001423.
[9]Prior D B, Bornhold B D, Wiseman W J, et al. Turbidity current activity in a British Columbia fjord[J].Science,1987, 237:1 330-1 333, doi: 10.1126/science.237.4820.1330.
[10]Garfield N, Rago T A, Schnebele K J, et al. Evidence of a turbidity current in Monterey Submarine Canyon associated with the 1989 Loma Prieta earthquake[J].Continental Shelf Research, 1994, 14:673-686, doi: 10.1016/0278-4343(94)90112-0.
[11]Khripounoff A, Vangriesheim A, Babonneau N, et al. Direct observation of intense turbidity current activity in the Zaire submarine valley at 4000 m water depth[J].Marine Geology,2003,194:151-158, doi:10.1016/S0025-3227(02)00677-1.
[12]Kinoshita K, Noble M A. The Monterey Submarine Canyon, California Moored Array Data Report[R].U.S. Geological Survey, 1995.
[13]Xu J P, Noble M A, Eittreim S L, et al. Distribution and transport of suspended particulate matter in Monterey Canyon, California[J].Marine Geology, 2002,181:215-234, doi:10.1016/S0025-227(0100268-7).
[14]Xu J P, Noble M A. Currents in Monterey Submarine Canyon[J].Journal of Geophysical Research, 2009,114, C03004, doi: 10.1029/2008JC004992.
[15]Paull C K, Ussler W III, Greene H G, et al. Caught in the act: The 20 december 2001 gravity flow event in Monterey Canyon[J].Geo-Marine Letters, 2003,22: 227-232, doi: 10.1007/s00367-003-0117-2.
[16]Xu J P, Noble M A, Rosenfeld L K. In-situ measurements of velocity structure within turbidity currents[J].Geophysical Research Letters, 2004,31: L09311, doi: 10.1029/2004GL019718.
[17]Xu J P. Normalized velocity profiles of field measured turbidity currents[J].Geology, 2010,38:563-566, doi: 10.1130/G30582.1.
[18]Normark W R, Piper D J W. Initiation processes and flow evolution of turbidity currents: Implications for the depositional record[C]∥Osborne R E, ed. From Shoreline to Abyss: Contributions in Marine Geology in Honour of Francis Parker Shepard. SEPM (Society for Sedimentary Geology) Special Publication,46,1991:207-230.
[19]Paull C K, Schlining B, Ussler W III, et al. Submarine mass transport within Monterey Canyon: Benthic disturbance controls on the distribution of chemosynthetic biological communities[C]∥Mosher D C, Craig Shipp, Lorena Moscardelli,
et al, eds. Submarine Mass Movements and Their Consequences: 4th International Symposium. New York: Springer,2009:229-246.
[20]Paull C K, Ussler W III, Johnson J E, et al. Recent sediment transport events in Monterey Canyon and fan channel[C]∥Geophysical Research Abstract: European Geosciences Union, 2006, 8:08799, abs. EGU06-A-08799.
[21]Paull C K, Caress D W, Ussler W III, et al. High-resolution bathymetry of the axial channels within Monterey and Soquel submarine canyons, offshore central California[J].Geosphere, 2011,7:1 077-1 101, doi:10.1130/GES00636.1.
[22]Smith D, Kvitek R, Iampietro P, et al. Twenty-nine months of geomorphic change in upper Monterey Canyon (2002-2005)[J].Marine Geology,2007,236(1/2): 79-94.
[23]Paull C K, Ussler W III, Caress D W, et al. Origins of large crescent-shaped bedforms within the axial channel of Monterey Canyon[J].Geosphere,2010, 6:755-774, doi: 10.1130/GES00527.1.
[24]Wynn R B, Piper D J W, Gee M J R. Generation and migration of coarse-grained sediment waves in turbidity current channels and channel-lobe transition zones[J].Marine Geology,2002,192:59-78.
[25]Xu J P, Wong F L, Kvitek R, et al. Sandwave migration in Monterey Submarine Canyon, Central California[J].Marine Geology, 2008,248/3-4:93-212. doi: 10.1016/j.margeo.2007.11.005.
[26]Xu J P, Barry J, Paull C K. Small-scale turbidity currents in a big submarine canyon[J].Geology, doi:10.1130/G33727.1,2013.
[27]Johnson K S, Paull C K, Barry J P, et al. A decadal record of underflows from a coastal river into the deep sea[J].Geology,2001, 29(11):1 019- 1 022.
[28]Piper D J W, Normark W R. Processes that initiate turbidity currents and their influence on turbidites: A marine geology perspective[J].Journal of Sedimentary Research, 2009,79:347-362,doi: 10.2110/jsr.2009.046.
[29]El-Gawad S M A, Pirmez C, Cantelli A, et al. 3-D numerical simulation of turbidity currents in submarine canyons off the Niger Delta[J].Marine Geology,
2012,326/328(C): 55-66,doi:10.1016/j.margeo.2012.06.003. |