[1] Galloway W E. Genetic stratigraphic sequences in basin analysis Ⅰ: ar-chitecture and genesis of flooding-surface bounded depositional units[J] .AAPG Bulletin, 1989a, 73:125~142
[2] Galloway W E. Genetic stratigraphic sequences in basin analysis Ⅱ: ap-plication to northwest Gulf of Mexico Cenozoic basin[J] . AAPG Bul-letin, 1989b, 73:143~154
[3] Frazier D E. Depositional.episodes: their relationship to the Quaternarystratigraphic framework in the northwestern portion of the Gulf basin[A] . The University of Texas at Austin, Bureau of Economic GeologyGeological Circular 74-1, 1974,28
[4] Xue Liangqing,Galloway W E. Sequence stratigraphic and depositionalframework of the Paleocene Lower Wilcox strata, Northwest Gulf ofMexico Basin[J] . Gulf Coast Association of Geological Societies Trans-actions, 1993,43: 453~464Xue Liangqing,Galloway W E. High-resolution depositional frameworkof the Paleocene middle Wilcox strata, Texas Coastal Plain[J] . AAPGBulletin, 1995, 79:205~230
[5] Meckel Ⅲ L D,Galloway W E. Formation of high-frequency sequencesand their bounding surfaces: case study of the Eocene Yegua Forma-tion, Texas Gulf Coast, USA[J] . Sedimentary Geology, 1996, 102:155~186
[6] Xue Liangqing. Depositional cycles and evolution of the PaleogeneWilcox strata, Gulf of Mexico Basin, Texes[J] . AAPG Bulletin,1997, 81:937~953
[7] Xue Liangqing, Galloway W E. Genetic sequence stratigraphic frame-work, depositional style, and hydrocarbon occurrence of the Upper Cre-taceous QYN Formations in the Songliao lacustrine basin, northeasternChina[J] . AAPG Bulletin, 1993, 77:1 792~1 808
[8] Swift D J P, Phillips S, Thorne J A. Sedimentation on continental mar-gins, V: parasequence[A] . In: SwiftDJ P, etal. eds. Shelfsand andsandstone bodies: geometry, facies and sequence stratigraphy[ C] . In-ternatinal Association of Sedimentologists, Special Pulblication 1991,12:153~187
[9] Haq B U, Hardenbol J, Vail P R. Mesozoic and Cenozoic chronos-tratigraphy and cycles of sea level change[A] . In: Wilgus C K, et al.eds. Sea level changes: an integrated approach[C] . SEPM, 1988,Special Publication 42:
[10] Hamilton D S, Tadros N Z. Utility of coal seams as genetic strati-graphic sequence boundaries in nonmarine basin: an example from theGunnedah basin, Austrinia[J] . AAPG Bulletin, 1994,78:267~286
[11] Aitken J F. Utility of coal seams as genetic stratigraphic sequenceboundaries in nonmarine basin: an example from the Gunnedah basin,Austrinia:discussion[J] . AAPG Bulletin, 1995,79:1 179~1 181
[12] Hamilton D S. Utility of coal seams es genetic stratigraphic sequenceboundaries in nonmarine basin: and example from the Gunnedahbasin, Austrania: reply[J] . AAPG Bulletin, 1995, 79:1 182
[13] Galloway W E. Paleogene depositional episodes, genetic stratigraphicsequences, and sediment accumulation rates, NW Gulf of Mexicobasin. Gulf Coast section[R] SEPM, llth Annual Research Confer-ence Proceedings. 1990, 165~176
[14] Galloway W E,Williams T A. Sediment accumulation rates in time andspace: Paleogene genetic stratigraphic sequences of the northwesternGulf of Mexico basin[J] . Geology, 1991, 19:986~989
[15] Liu X, Galloway W E. Quantitative determination of Tertiary sedi-ment supply to the North Sea Basin[J] . AAPG Bulletin, 1997, 81:1482~1509