[1] |
1.贾蓉芬,林本海.西安段家坡黄土有机质特征及其环境意义.地理科学,1993.13(4):337-345. 2.刘东生等.黄土与环境.北京:科学出版社,1985.191-302. 3.刘鑫麒.渭南黄土剖面的年龄侧定及十五万年来高分辨时间序列的建立.第四纪研究,1994. (3) :193-202. 4.刘友梅等.黄土中元素组分演化的阶段性、周期性和古气候变化.地球化学,1987, (4) :381-388. 5.么枕生.气候学原理.北京:科学出版社,1959.361-379. 6.潘裕焕.生产过程自动化中的数学模型.北京:科学出版社,1977.226-227. 7.文启忠等.黄土剖面中古气候变化的地球化学记录.第四纪研究,1995. ( 3 ) : 223-231. 8.徐道一等.天文地质学概论.北京:科学出版社,1983.162. 9.杨蔚华,刘友梅.地球化学中某些数学模型的探讨.地球化学文集,北京:科学出版社,1986. 319-324. 10.Agterberg F P. Geomathematic. Eiserier Scientific Publishing Company. Amsterdam-London-New York. 1974.363-400. 11.Berger A. Molankovitch and climate. Reviews of Geophysics. 1988. 26:624-657. 12.Ihvis J C. Statistics and Ihta Analysis in Geology. New York. 1973. 170-294. 13.Hays J D. Variations in the Earth's orbit:Pacemarker of the Ice Ages. Science. 1976. (194):1121-1132. 14.Milankovitch M M. Kanon der Erdbestrahiung. I3eograd. Koningglich Serbische Akademie, 1941. 484. 15.Komiru M A and Pisla N G. Pleistocene climate:deterministic or stochastic? Science. 1979. (204):171-173. 16.Shackleton N J.Ocygen-isotope and Paleomagnetic stratigraphy of equatorical Pacificcore.V28-239: to Latest Pleaistocene. Geol. Soc. Amer. Memr.1976,449-462. |