[1] 夏文杰、杜森官、徐新煌等著,中国南方震旦纪岩 相古地理与成矿作用[M] .北京:地质出版社.1994.1~12
[2] Wignall, P.B., Black shales[M] . Oxford: Clarendon Press. 1994 . 24~28
[3] Nuhfer, E.B., Mudrock fabrics and their significance-discussion[J] . Journal of Sedimentary Petrology, 1981, 51: 1 027~1 029
[4] Pye K, Krinsley D H. Microfabric, mineralogy and early diag enetic his tory of the Whitby Mudstone Formation(Toarican), Cleveland Basin[J] , UK. Geolo gical Magazine,1986, 123: 191~203
[5] Leckie D A, Singh C, Goodarzi F, Wall J H. Organic-rich, radioacti ve marine shale: a case study of a shallow-water condensed section, Cretaceous S haftesbury formation, Alberta, Canada[J] . Journal of Sedimentary Petrology, 19 90, 60: 101~117
[6] O'Brien N R. Significance of lamination in Toarcian(Lower Jurassic )shales from Yorkshire, Great Britain[J] . Sedimentary Geology, 1990, 67: 25~3 4
[7] Banerjee I, Kidwell S M. Significance of molluscan shell be ds in sequ ence stratigraphy: an example from the Lower Cretaceous Maunville Group of Canad a[J] . Sedimentology, 1991,38:913~934
[8] Coveney R M Jr, Watney W L, Maples C G. Contrasting depos itional mo dels for Pennsylvanian black shale discerned from molybdenum abundances[J] . Ge ology, 1991,19: 147~150
[9] Jervey M T. Quantitative geological modeling of siliceous clastic rock sequ ences and their seismic expression. In:Wilgus C K,et al,eds.Sea-level change s: an integrated approach [C] , SEPM Special Publication, 1988,42:47~70
[10] 张爱云,伍大茂,郭丽娜,王云龙著,海相黑色页岩建造地球化学与成矿意 义[M] .北京:科学出版社,1987:20~60
[11] 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[J] .地质科学, 1994, 29(1):41~54
[12] 刘宝王 君,许效松著, 中国南方古大陆沉积地壳演化与成矿[M] .北京: 科学出版社, 1993:61~65
[13] Creaney, S., and Passey, Q.R. Recurring paterns of total organic c arbon and source rock quality within a sequence stratigraphic framework[J] , AAPG Bulleti n, 1993,77:386~401.
[14] 杨卫东,肖金凯,于炳松等滇黔磷块岩沉积学、地球 化学与可持续开发战略[M] .北京:地质出版社,1997:76~86
[15] Batnrin, G.N., Stages of Phosphorite formation on the ocean floor[J], Nature, 1971, 232: 61~62.
[16] 范德廉,杨秀珍,王连芳等,某地下寒武统含镍钼多元素黑色岩系的 岩石学及地球化学特点[J] .地球化学,1973, 3:143~165