[1] |
1 王东安.扬子地台晚元古代以来硅岩地球化学特征及其成因.地质科学, 1994, 29(1):41~54 2 谢窦克.皖南浙西上震旦统碧玉岩的地质意义.中国地质科学院南京地质矿产研究所刊, 1979 3 Brassell S C. Applicat ions of bi omarkers for delineating marine paleoclimatic flutuat ions during the Pleistocene.In :Engel M H, Macko S A, eds Organic Geochemi stry Principles and Applications.Plenum Press, 1993.699~738 4 Fu Jiamo, S heng Guoying, Xu Jiayou, Eglinton G, Gow ar A P, Jia Rongfen, Fan Shanf a, Peng Pingan.Application of biological markersin the assessment of paleoenvi ronment s of Chinese non -marine sediments.Org.Geochem, 1990, 16 :769~770 |