TURBIDITY CURRENTS AS A CAUSE OF GRADED BEDDING

[1] Bailey E.B., 1930, GEOL MAG, V67, P77

[2] BAILEY EB, 1938, GEOL SOC GLASGOW T, V20, P1

[3] BAILEY EB, 1936, GEOLOGICAL SOC AM B, V47, P1713

[4] Density currents as agents for transporting sediments [J]. JOURNAL OF GEOLOGY, 1942, 50 (05) : 512 - 547

[5] BLACKWELDER E, 1928, GEOLOGICAL SOC AM B, V39, P465

[6] Boswell P.G.H., 1930, GEOL MAG, V67, P371

[7] BRAMLETTE MN, 1940, 196A US GEOL SURV PR, P1

[8] DALY RA, 1942, FLOOR OCEAN NEW LIGH

[9] FOSSAMANCINI E, 1922, SOC GEOL ITALIANA B, V41, P126

[10] FRASER HJ, 1929, ROYAL SOC CANADA T, V23, P49

[1] Bailey E.B., 1930, GEOL MAG, V67, P77

[2] BAILEY EB, 1938, GEOL SOC GLASGOW T, V20, P1

[3] BAILEY EB, 1936, GEOLOGICAL SOC AM B, V47, P1713

[4] Density currents as agents for transporting sediments [J]. JOURNAL OF GEOLOGY, 1942, 50 (05) : 512 - 547

[5] BLACKWELDER E, 1928, GEOLOGICAL SOC AM B, V39, P465

[6] Boswell P.G.H., 1930, GEOL MAG, V67, P371

[7] BRAMLETTE MN, 1940, 196A US GEOL SURV PR, P1

[8] DALY RA, 1942, FLOOR OCEAN NEW LIGH

[9] FOSSAMANCINI E, 1922, SOC GEOL ITALIANA B, V41, P126

[10] FRASER HJ, 1929, ROYAL SOC CANADA T, V23, P49