[1] 1 O'Neil J R, Clayton R N.Mayada T K.Oxygen isotope fmc-donation in divalent metal carbonates.,J Chiem Phys, 1969-51(12): 5547- 5558.

2 汪训一桂林洞穴沉积物的氧碳同位素特征.中国岩溶. 1985.4(1): 149- 154.

3 Hendy C H The isotopic geochemistry of speleochems-I The calculation of the effects of different modes of formation on theisotopc composition of spelesthems and their applica- bility as palaeoclimaticindicators. Geochim Commochim Ac- ta, 1971, 3S 801-824.

4 陈跃.黄培华.朱洪山.北京周口店地区洞穴内第四纪石笋的同位素古温度研究.科学通报.1986, 31(20): 1576-1578

5 Craig H Isotopic variations in meteroicwater Science, 1961, 133 1702- 1703

6 Epstein S, Sharp R P. Antareticice sheet stabe isotope analy-ses of Byrd station cores and interhemispheric climatic implica-lions. Science, 1970, 16& 1570- 1572.

7 王建生.虞福基.刘德平.中国东部人气降水氢、氧同位素组成.地球化学.1987.(1): 22- 26.

8 王兆荣.壳慢演化与成岩成矿同位素地球化学.北京:科学出版社.1993. 11 220.

9 陈明.本世纪80年代中国东南沿海第四纪地质研究的进展.地质论评.1991, 37 ( 4): 378- 379.