A Lower Permian sandwave-containing shelf sequence exposed at Zungwini Mountain, Republic of South Africa

[1]  P. Harris.  Large-scale bedforms as indicators of mutually evasive sand transport and the sequential infilling of wide-mouthed estuaries , 1988 .

[2]  A. Smith,et al.  Early Permian giant cross-beds near Nqutu, South Africa, interpreted as part of a shoreface ridge , 1988 .

[3]  S. Berné,et al.  Internal structure of subtidal sandwaves revealed by high‐resolution seismic reflection , 1988 .

[4]  A. Smith,et al.  The Ecca-Beaufort transition zone near Philipstown, Cape Province: a marine shelf sequence , 1988 .

[5]  W. L. Duke.  Hummocky cross-stratification, tropical hurricanes, and intense winter storms , 1987 .

[6]  R. Dott,et al.  Depositional Facies and Progradational Sequences in Eocene Wave-Dominated Deltaic Complexes, Southwestern Oregon , 1986 .

[7]  T. R. Mason,et al.  Palaeoevironmental significance of ichnogenus Diplocraterion torell from the Permian vryheid formation of the Karoo Supergroup, South Africa , 1986 .

[8]  D. Swift,et al.  Barrier island evolution, middle Atlantic shelf, U.S.A. Part I: Shoreface dynamics , 1985 .

[9]  P. Allen.  Hummocky cross-stratification is not produced purely under progressive gravity waves , 1985, Nature.

[10]  B. Cairncross,et al.  High-constructive lobate deltas in the Lower Permian Vryheid Formation, Rietspruit, South Africa , 1984 .

[11]  E. King,et al.  Bedforms of the Canadian eastern seaboard: A comparison with global occurrences , 1984 .

[12]  P. Allen,et al.  Evolution and mechanics of a Miocene tidal sandwave , 1984 .

[13]  D. Swift,et al.  Hummocky Cross-Stratification and Megaripples: A Geological Double Standard? , 1983 .

[14]  R. Dott,et al.  Hummocky stratification: Significance of its variable bedding sequences , 1982 .

[15]  R. Tavener-Smith.  Prograding coastal facies associations in the Vryheid formation (Permian) at Effingham quarries near Durban, South Africa , 1982 .

[16]  T. Aigner.  Calcareous Tempestites: Storm-dominated Stratification in Upper Muschelkalk Limestones (Middle Trias, SW-Germany) , 1982 .

[17]  John M. Huthnance,et al.  On one mechanism forming linear sand banks , 1982 .

[18]  P. Allen,et al.  Wave-, tide-, and current-controlled sandbodies of miocene molasse, western Switzerland , 1981 .

[19]  D. Cacchione,et al.  Sand waves on an epicontinental shelf: Northern Bering Sea , 1981 .

[20]  J. Terwindt,et al.  Neap–spring tide sequences of intertidal shoal deposits in a mesotidal estuary , 1981 .

[21]  J. R. Allen.  Sand waves: A model of origin and internal structure , 1980 .

[22]  B. W. Flemming,et al.  Sand transport and bedform patterns on the continental shelf between Durban and Port Elizabeth (southeast African continental margin) , 1980 .

[23]  N. W. Lanfredi,et al.  Shoreface-connected sand ridges on American and European shelves: A comparison , 1978 .

[24]  P. Mccabe,et al.  Deep distributary channels and giant bedforms in the Upper Carboniferous of the Central Pennines, northern England , 1977 .

[25]  D. Hobday,et al.  Storm beach deposits in the late Palaeozoic Ecca Group of South Africa , 1977 .

[26]  J. Ludwick.  Tidal Currents and Zig-Zag Sand Shoals in a Wide Estuary Entrance , 1974 .

[27]  H. Reineck,et al.  Depositional sedimentary environments , 1973 .

[28]  A. L. Toit,et al.  The geology of South Africa , 1927 .