| [1] | Pystawalov, L. B.，1956, Secondary change of sedimentary rocks and their significance. Tr. GeoI, Akad. Nauk SSSR, I9-22. |
| [2] | Rahmani, R.A, 1973, Grain surface etching feature of some heavy minerals.J. Sediment. Petrol, V. 43, 882-888. |
| [3] | Morton, A.C.，1984, Stability of detrital heavy minerals in Tertiary sand-stops from the North Sea Basin. Clay Minerals, V.19, 287-308. |
| [4] | Franks, S, G.，I984, Relationships among carbon dioxide, pore-fluid the-mistry, and secondary porsity, Texas Gulf Coast(abs.).Bull. Am. Ass-oc. Pet. Geol. V .68, 478. |
| [5] | Hazeldine, R.S.，1984, Quartz diagenesis and convective fluid movement, Beatrice Oilfield, UK. North ,'Sea. Clay Minerals, V. 19, 391-402. |
| [6] | Hoffman, J. and Hower, J.，1979, Clay mineral assemblies as low grade metamorphic geothermometerss Application to the thrustfaulted disturbed Belt of MontanaU.S.A.，SEPM, Special Publication, V. 26,35-79. |
| [7] | Hower, J.，Eslinger, E, V.，Hower, M. E. and Perry, E. A.，1976, Me-chanism of argillaceous sediments, Mineralogical and chemical evidence.Bull. Geol. Soc, Amer. 87, 725-737. |
| [8] | Surdam, R, C, 1984,Mineral oxidants and porosity enhancement. Bull. Am-er. Assoc. Pet. Geol. V.68, p. 523. |