[1]王江海等.耗散结构理论在混合岩研究中的应用.地学探索，1988,  1  (1): 8-15
[2]吴金平、王江海.硅酸盐固溶体矿物中组分的韵律型空间分布及形成过程的时空自组织.矿物学报,1990, 10(3):193-203
[3]王江海等.福建镇海一带玄武岩柱状节理的动力学兼论柱状节理的成因.岩石学报，1991,  7 (1)：16-25
[4]Wang Jianghai et al.，the rhythmic spatial distribution and self一organization of components in silicate-solid一solution minerals.  Chinese J,  of Geochemistry,  1991，3  (in  press)
[5]王江海等.斜长石振荡环带成因的动力学模型.地质科技情报，1990,  9  (2)：51-57
[6]郑在胜.岩石变形中的能量传递过程与岩石变形动力学分析.中国科学(B辑)，1990,  5: 52A-537.
[7]王江海.大别杂岩的早期演化兼论混合岩成因机制.中国地质大学出版社，1991(印刷中)
[8] Boss,A. P. et al. ,Time-dependent models of single and double一layer mantle convection. Nature ,1989 , 308: 533一535
[9]Huppert,H. E. et al. ,Emplacement and cooling of komatiite lavas. Nature, 1989,309;19一22
[10]Jaupart,C. et al.,SG3gnant layers at the bottom of connecting magma chambers. Nature,1984,308:535一538.
[11]Mc Dougall,T J. et al. ,Fluid dynamic implications for massive sulphide deposits of not saline fluid flowing into a submarine depression from below. Deep-Sea Res.，1984,31(2):145一170.
[12]Norton, D. ,et al. ,Quantitative simulation of the hydrothermal systems of crystallizing magmas on the basis of transport and oxygen isotope data;An analyses of the Skaergaard intrusion. J. Petrol.，1979,20:421-986
[13]Ortoleva, P. ,The self一organization of Liesegang bands and other precipitate patterns,in; G. Nicolis and F.13aras(eds)，Chemical Instabilities.D.Reidel Publishing Company,1984 ; 289-298,329-340
[14]Spera,F J. et al. ,Double-diffusive convection in magma Chambers;Single of multiple Iayers7,Geophys. Res. Lett.，1986, 13(1):153-156
[15] Turner,J. S. ,A Fluid dynamlcal model of differentiation and layering in chambers. Nature ,1980 , 285:213-215
[16]Turner, J. S. et al. ,7.'rie flow of hot saline solutions from vents in sea floor一some implications for exbatative massive sulphide and other ore deposits,Econ. Geol. ,T3,1978:1082-1100
[17] Huppert,H. E. A Latxmatory model of a replenished magma chamber,Farth Planet. Sci. )..eit. 1981;54:144一152
[18]Haase,C'. S. et al. ,Oscillatory zoning in plagiodase feldspar. Science,1980; 209:272一274.
[19]李如生.岩浆岩中旷物组分分布的有序现象和耗散结构.矿物学报，1989;9:303 - 310
[20]放崇文.地球化学的理论体系与方法论.地球科学，1986,11(4):331一339
[21]聆崇文.成矿作用与耗散结构.地质学报，1987;61(4):336 - 349
[22]龄崇文.成矿作用的动力学体系.现代地质，198913:267- 289
[23]放崇文等.云南个}日成矿区锡石一硫化物矿床原生金属分带形成的动力学机制.地质学报，1990;69(3)226- 237
[24]Ortoleva,P. et al. ,Geochemical Self一organization I and II,Am. J. Sci.，19871287:979-1040
[25]Dewers,T. and Ortoleva,P. ,A coupled reaction一transport一mechanical model for intergranular pressure solution,stylolites and differential compaction and cementation in clean sand stone,Geochimica et cosmochimica Acta,1990; 54(6):1609-1625
[26] Kantha,L. H. Basalt fingers-origin of columnar joints. Geol. Magzine,1981;118(3):251-269
[27] Beiersdorf,H. et al.，饶雪峰等译(1991)，成岩层理和纹层，国外地质1986; 2; 32-36
[28] McBirney et al,Ctystallization and layering of the Skaergaard intrusion. J. of Petrol. ,1979;20(3):487-554
[29] Boudreau,A. E. ,examples of patterns in igneous rocks,in Nicolis,G. ,Baras,F. (eds),Chemical Instabilities. D. Reidel Pub-lishing Company,1984; 299-304.
[30]Ortoleva,P. et al. ,Kinetics of metamorphiclayering in anisotropically stressed rocks .Am. J. Sci. ,1982 ; 282: 619-693