[1] |
(1)周中毅等,(1919)碳酸盐岩中有机质的热变实验。中国科学院地球化学研究听年报, 1978-197 9),66-68页。 (2)郝石生,(1982)华北地区震旦亚界古地温演化及冀中地1原生油气藏形成条件初探,华东石油学院学报,1,1-170 (3) 张子枢,(1980)成熟度的化学及矿物学指标分类,地质地球化学,922-290 (4) 浅川忠(1979)泥质岩 -碳酸盐岩沉积阶段和油气的生成、运移、聚集与压实特征之间的关系,石油地质实验,4,1-220 (5) Waples, D.W.,(1980)Time and Temperature in Petroleum Formation:Application of Lopatin's Method to Petroleum Exploration, BuII.AAPG.V.64 N.6 (6) Tissot,B.B.,and Welte, D.H.,(1978)Petroleum Formation and Occurre-nce, Nnw York (7) Cooper, B.S·,(1977)Estimaiion of the Rlasimum Temperatures Attained in Sedimeniary一Rock,Dcvclopments in Petrolcun Geology-I, London,Applied Science Pub. (8) Connan, J.,(1974)Time一Temperature Relation in Oil Genesis,Bull.AAPG,V.58 N.12 (9)Hood, J·,et al.,(1975)Organic Metamorphism and the Generation of Petr-oleum, Bull.AAPG.V. 59N.6 (10)Veto, I.,(1979)An Exmination of the Timing of Catagenesis of Organic Matter Using Three Published Methods ,Advarrces in Organic Gcochcmistry |