[1] 1 居春荣,刘震. 曹冰苏北盆地高邮凹陷下第三系层序地层划分及油藏分布特征[J].现代地质,2003,(z1):24-27.

2 HarLandW,Cox A V. A geologic time scale[M].London: Cambride University Press,1982.76-83.

3 江苏省地质矿产局. 江苏省及上海市区域地质志[M].北京:地质出版社,1984.

4 梅冥相. 碳酸盐岩旋回与层序[M].贵阳:贵州科学技术出版社,1995.92-148.

5 HuangXingzhen,Yang Xiaorong,Shao Hongshun,Lei Zhenfeng. The carbonate deposits of lacustrine facies, an example from the Tertiary of the Qaidam Basin[J].China Earth Sciences,1990,(03):241-251.

6 黄杏珍,阎存凤,王随继. 苏打湖型的湖相碳酸盐岩特征及沉积模式[J].沉积学报,1999,(Z1):728-733.

7 黄杏珍,邵宏舜,阎存凤. 泌阳凹陷下第三系湖相白云岩形成条件[J].沉积学报,2001,(2):207-213.

8 HuangXingzhen,Shao Hongshun,Lei Zhenfeng. The relationship between carbonate sedimentation and salinity in brackish lake basin Chinese Academy of Sciences, Developments in Geoscience[M].北京:科学出版社,1989.319-327.

9 纪友亮,张世奇. 层序地层学原理及层序成因机制模式[M].北京:地质出版社,1998.46-63.

10 VailPR. Seismic stratigraphy and global changes of sea level[Z].AAPG Memoir,1977.63-82.

11 VailPR,HardenbolJ. Sea-level changes during the Tertiary[J].Ocean,1979.77-79.

12 王英华. 鲕粒与沉积环境[A].北京:北京大学出版社,1982.