| [1] |
(1) 晋惫娟、李育慈，1989,博格达山西南麓晚古生代风暴岩一半深海块体搬运沉积物及其形成的构造背景，沉积学报增刊，7-20页 (2) 宋春晖、晋慧娟，1989，博格达t1」北越下二叠统石人子沟组碎屑流和高密度蚀流沉积的类型及演化，沉积学报增刊，80-107页 (3) 中国科学院地学部，新班石油管理局，1989,准噶尔盆地形成演化与油气形成，科学出版社，56-70页. (4) Duke W. L.，1985, Hummocky Cross- stratification, Trppical Hurricanes and Intense wind Storms. Sedimentology, V.32, N.2, p.167-194. (5) Bourgeois J., 1980, A Transgressive Shelf Sequence Exhibiting Hunmocky stratification: The Cape sebastion Sand- stone (upper cretaceous) Southwestern Oregen. J. Sed. Petrol., V.S, N.3, p.681-702 (6) Prave A. R. and W. L. Duke.，1990, SmaV-Scale Hummocky Cross-Stratification in Turbidites: a Form of Antidune stratification, Sedimentology, V.37, N.3, p.531-539 (7) Jackson M. J., Simpson and K. A. Eriksson, 1990, Facies and sequence stratigraphic analysis in an intracratonic. therma]一relaxation basin: the Early Proterozoic Lower Quilarlar Formation and Ballara Quartile. Mount Isa Inlier, Australia. Sedimentology, V.37, N.6, p.1053-1078. |