[1] |
Ourisson G. Frontiers of organic geochemistry: some unresolved proble ms[J] . Org. Geochem., 1990, 16(1-3): XXI~XXIV |
[2] |
Freeman K H, Hayes J M, Trendel J, et al., Evidence from carbon isot ope measurements for diverse origins of sedimentary hydrocarbons[J] . Nature, 1990,343:254~256 |
[3] |
Schoell M, McCaffrey M A, Fago F J. et al., Carbon isotopic comp ositi ons of 28, 30-bisnorhopanes and other biological markers in a Monterey crude oil [J] . Geochim. Cosmochim. Acta,1992, 56: 1 391~1 399 |
[4] |
Bjoroy M, Hall P B, Hustad E, et al., Variation in stable carbon isot ope ratios of individual hydrocarbons as a function of artificial maturity[J] . Org. Geochem. 1992, 19(1-3): 89~105 |
[5] |
周友平,史继扬,向明菊,屈定创.沉积有机质中藿烯的成因研究-碳稳定同位 素证据[J] .沉积学报,1998,16(2):14~19 |
[6] |
Ourisson G. The microbial origin of fossil fuels[J] . Scientific A merican, 1984, 251(2): 34~41 |
[7] |
史继扬,向明菊,洪紫青等.五环三萜烷的物源和演化[J] . 沉积学报(专刊),1991.26~33 |
[8] |
Quirk M M, Wardroper A M K, Wheatley R E, et al. Extended hopan oids in peat environments[J] .Chemical Geology, 1984, 42: 25~43 |
[9] |
Maowen Li, Johns R B, Bowen Mei. A study in early diagenes is: Bi omarker composition of a suite of immature coals and coaly shales[J] .Org. Geo chem.1990, 16(4-6): 1 067~1 075 |
[10] |
Rohmer M, Dastillung M, Ourisson G. Hopanoids from C30 to C3 5 in recent muds[J] . Nature,1980, 67: 456~458 |