[1] 1.Demicco R V and Spencer R J. MAPS一a 13AS1C program to model accumulation of platform sediments. Computer and Geosciences, 1989. 15 (1):95-105.

2.Spencer R J and Demicco R V. Computer models of carbonate platform cycles driven by subsidence and eustasy. Geolo-gy. 1989. 17: 165-168.

3.Hays 1 D. Imbrie 1 and Schackleton N J. Variation in the earth's orbit: pacemaker of the ice ages. Science, 1976. 194:1121.

4.Goldhammer R K. Dunn P A and Hardie I. A. High frequency glacio一eustatic sea level oscillation with Milankovitch characteristics recorded in Middle Triassic plat form carbonates in N. Italy. Am. Jour, Science. 1987, 287:853-892.

5.Goldhammer R K. Dunn P A and Hardie I. A. Depositional cycles, composite sea level changes, cycle stacking pattens. and the hierarchy of stratigraphic forcing: examples from Alpina Triassic Platform carbonates. Geological Society of America BuVetin. 1990. 102: 535.

6.Koerschner,,W F and Read J F. Field and modelling studies of Cambrian carbonate cycles. Virginia Appalachians.J. Sedment. Petrol.,1989. 59 (3):654-687.

7.Olsen P E. A 40一mivon一year lake record of Early Mesozoic orbital climatic forcing. Science. 1986, 234:842-848.

8.Schlager W. The paradox of drowned reefs and carbonate platform. Geo. Soc. Am. Bull.,1981, 92: 197-211.

9.于炳松.塔里木盆地北部寒武纪海平面变化研究.沉积学报,1996. 14 (1) : 33-39.

10. 于炳松.塔里木盆地北部中下奥陶统碳酸盐岩陆拥—盆地的层序地层分析.矿物岩石,1995. 15 (3): 44-49.