[1] 1 湖南地质矿产局，1988,湖南省区城地贡志，北京:地质出版社。

2 广西地质矿产局，1985.广西壮族自治区区城地质治.北京:地质出版社。

3 曾允孚等.1987，南岭泥盆系层控矿床，北京:地质出版社。

4 BorId,G. C.，et al.，1989, Role of thermal subsidencs. flexure. and eustasy in the evolution of early PaLuroaoic passive一margin carbomte platform. SEPM Special Publication, N. 44, p. 39一61.

5 Crevello, P. D. et al.，Controls on Carbomte Platform end Basin Development. SEPM Special Publication, N. 44.

6 Mull . A. D.，1990. Principles of Sedimentary Basin Amlysis. Springer-Verlag.

7 Tucker，M. E. et al.，1990, Carbomte Platform, faciea, sequences and evolution. Blackwell Scientific Publication.

8 Fasamentier. H. W. et al, Ecstatic rnntrols on cleatic deposition I-rnnceptual framework. SEPM Special Publication.N.42.

9 Van Wagoner. J. E. et al, 1988, An overview of the fundamental of sequence atratigraphy and key definition. in Wilgus,C. K. et al . (Sea Level Changes一An Integrated Apprach) SEPM Sepcial Pubiicstion.

10 Vail, P. R. et al.，1984. Jurassic unconformities. chromtratigraphy, and sea level changes from seismic atratigraphy and bioatratigraphy, in J. S. Schlee. ed.，lnterregioml unconformities and hydrocarbon accumulation, AAPG Memoir 36.