REFERENCES
129
Spencer, A. M. (1971). "Late PreCambrian Glaciation in Scotland," Mem. No. 6. Geol. Soc. London, London. 100pp.
Stanley, D. J., and Unrug, R. (1972). Submarine chan:lel deposits, Fluxoturbidites and other indicators of slope and base of slope environments ire modern and ancient marine basins. Spec.
Publ.- Soc. Econ. PaleontoL MineraL, 16, 287-34~'.
Stauffer, E H. (1967). Grainflow deposits and their illaplications, Santa Ynez Mountains, California. J. Sediment. Petrol 37, 487-508.
Stow, D. A. V. (1985). Deep-sea clastics: Where are we and where are we going? In "Sedimentology: Recent Developments and Applied Aspecls" (E J. Brenchley and B. E J. Williams,
eds.), pp. 67-94. Blackwell, Oxford.
Stow, D. A. V. (1986). Deep clastic seas. In "Sedimentary Environments and Facies" (H. G. Reading, ed.), 2nd ed., pp. 399-444. Blackwell, Oxford.
Stow, D. A. V., and Lovell, J. E B. (1979). Contourites: Their recognition in modern and ancient
sediments. Earth Sci. Rev. 14, 251-291.
Stow, D. A. V., Reading, H. G., and Collinson, J. D. (1996). Deep seas. In "Sedimentary Environments: Processes, Facies and Stratigraphy" (H. G. Reading, ed.), 3rd ed., pp. 395-453.
Blackwell, Oxford.
Sundborg, A. (1956). The River Klar~ilven, a study in fluvial processes. Geogr. Ann. v. 38, 127316.
Suthren, R. J. (1985). Facies analysis of volcaniclastic sediments: A review. In "Sedimentology:
Recent Developments and Applied Aspects" (E J. Brenchley and B. E J. Williams, eds.),
pp. 123-146. Blackwell, Oxford.
Tsoar, H., and Pye, K. (1987). Dust transport and the question of desert loess formation. Sedimentology 34, 139-153.
Van der Lingen, G. J. (1969). The turbidite problem. N.Z.J. Geol. Geophys. 12, 7-50.
Vanoni, V. A. (1964). "Measurements of Critical Shear Stress for Entraining Fine Sediments in
a Boundary Layer," W. M. Tech Lab. Rep. K. H.--R--7. California Institute of Technology,
Pasadena. 47pp.
Van Straaten, L. M. J. U. (1964). Turbidite sediments in the southeastern Adriatic Sea. In "Turbidites" (A. H. Bouma and A. Brouwer, eds.), pp. 142-147. Elsevier, Amsterdam.
Varnes, D. J. (1958). Landslide types and processes. Spec. Rep.--Natl Res. Counc., Highw. Res.
Board 29 (544), 20-47.
Visser, M. J. (1980). Neap-spring cycles reflected in Holocene subtidal large-scale bedform deposits: A preliminary note. Geology 8, 543-546.
Walker, R. G. (1965). The origin and significance of the internal sedimentary structures of turbidites. Proc. Yorks. Geol. Soc. 35, 1-32.
Walker, R. G. (1967a). Turbidite sedimentary structures and their relationship to proximal and
distal depositional environments. J. Sediment. Petrol 37, 25-43.
Walker, R. G. (1967b). Upper flow regime bedforms in turbidites of the Hatch Formation, Devonian of New York State. J. Sediment. Petrol 37, 1052-1058.
Walker, R. G. (1970). Review of the geometry and facies organization of turbidites and turbiditebearing basins. Spec. Pap.- Geol. Assoc. Can. 7, 219-251.
Weaver, E E E., Masson, D. G., and Kidd, R. B. (1994). Slumps, slides and turbidity currentssea-level change and sedimentation in the Canary basin. Geoscientist 4 (1), 14-16.
Whetten, J. T. (1965). Carboniferous glacial rocks from the Werrie Basin, New South Wales, Australia. Geol. Soc. Am. Bull 76, 43-56.
Williams, G. (1964). Some aspects of the eolian saltation load. Sedimentology 3, 257-287.
Wilson, I. G. (1971). Desert sandflow basins and a model for the development of Ergs. Geogr. J.
137, 180-199.
Wilson, I. G. (1972). Aeolian bedforms-their development and origins. Sedimentology 19, 173210.
Zeng, K. W., and Lowe, D. R. (1997a). Numerical simulation of turbidity current flow and sedimentation: 1. Theory. Sedimentology 44, 67-84.
Zeng, K. W., and Lowe, D. R. (1997b). Numerical simulation of turbidity current flow and sedimentation: 2. Results and geological application. Sedimentology 44, 85-104.
129
Spencer, A. M. (1971). "Late PreCambrian Glaciation in Scotland," Mem. No. 6. Geol. Soc. London, London. 100pp.
Stanley, D. J., and Unrug, R. (1972). Submarine chan:lel deposits, Fluxoturbidites and other indicators of slope and base of slope environments ire modern and ancient marine basins. Spec.
Publ.- Soc. Econ. PaleontoL MineraL, 16, 287-34~'.
Stauffer, E H. (1967). Grainflow deposits and their illaplications, Santa Ynez Mountains, California. J. Sediment. Petrol 37, 487-508.
Stow, D. A. V. (1985). Deep-sea clastics: Where are we and where are we going? In "Sedimentology: Recent Developments and Applied Aspecls" (E J. Brenchley and B. E J. Williams,
eds.), pp. 67-94. Blackwell, Oxford.
Stow, D. A. V. (1986). Deep clastic seas. In "Sedimentary Environments and Facies" (H. G. Reading, ed.), 2nd ed., pp. 399-444. Blackwell, Oxford.
Stow, D. A. V., and Lovell, J. E B. (1979). Contourites: Their recognition in modern and ancient
sediments. Earth Sci. Rev. 14, 251-291.
Stow, D. A. V., Reading, H. G., and Collinson, J. D. (1996). Deep seas. In "Sedimentary Environments: Processes, Facies and Stratigraphy" (H. G. Reading, ed.), 3rd ed., pp. 395-453.
Blackwell, Oxford.
Sundborg, A. (1956). The River Klar~ilven, a study in fluvial processes. Geogr. Ann. v. 38, 127316.
Suthren, R. J. (1985). Facies analysis of volcaniclastic sediments: A review. In "Sedimentology:
Recent Developments and Applied Aspects" (E J. Brenchley and B. E J. Williams, eds.),
pp. 123-146. Blackwell, Oxford.
Tsoar, H., and Pye, K. (1987). Dust transport and the question of desert loess formation. Sedimentology 34, 139-153.
Van der Lingen, G. J. (1969). The turbidite problem. N.Z.J. Geol. Geophys. 12, 7-50.
Vanoni, V. A. (1964). "Measurements of Critical Shear Stress for Entraining Fine Sediments in
a Boundary Layer," W. M. Tech Lab. Rep. K. H.--R--7. California Institute of Technology,
Pasadena. 47pp.
Van Straaten, L. M. J. U. (1964). Turbidite sediments in the southeastern Adriatic Sea. In "Turbidites" (A. H. Bouma and A. Brouwer, eds.), pp. 142-147. Elsevier, Amsterdam.
Varnes, D. J. (1958). Landslide types and processes. Spec. Rep.--Natl Res. Counc., Highw. Res.
Board 29 (544), 20-47.
Visser, M. J. (1980). Neap-spring cycles reflected in Holocene subtidal large-scale bedform deposits: A preliminary note. Geology 8, 543-546.
Walker, R. G. (1965). The origin and significance of the internal sedimentary structures of turbidites. Proc. Yorks. Geol. Soc. 35, 1-32.
Walker, R. G. (1967a). Turbidite sedimentary structures and their relationship to proximal and
distal depositional environments. J. Sediment. Petrol 37, 25-43.
Walker, R. G. (1967b). Upper flow regime bedforms in turbidites of the Hatch Formation, Devonian of New York State. J. Sediment. Petrol 37, 1052-1058.
Walker, R. G. (1970). Review of the geometry and facies organization of turbidites and turbiditebearing basins. Spec. Pap.- Geol. Assoc. Can. 7, 219-251.
Weaver, E E E., Masson, D. G., and Kidd, R. B. (1994). Slumps, slides and turbidity currentssea-level change and sedimentation in the Canary basin. Geoscientist 4 (1), 14-16.
Whetten, J. T. (1965). Carboniferous glacial rocks from the Werrie Basin, New South Wales, Australia. Geol. Soc. Am. Bull 76, 43-56.
Williams, G. (1964). Some aspects of the eolian saltation load. Sedimentology 3, 257-287.
Wilson, I. G. (1971). Desert sandflow basins and a model for the development of Ergs. Geogr. J.
137, 180-199.
Wilson, I. G. (1972). Aeolian bedforms-their development and origins. Sedimentology 19, 173210.
Zeng, K. W., and Lowe, D. R. (1997a). Numerical simulation of turbidity current flow and sedimentation: 1. Theory. Sedimentology 44, 67-84.
Zeng, K. W., and Lowe, D. R. (1997b). Numerical simulation of turbidity current flow and sedimentation: 2. Results and geological application. Sedimentology 44, 85-104.