[1] 於崇文. 地球化学系统的复杂性探索. 地球科学, 1994, 19(3) : 283~286. [2] 於崇文. 地球化学动力学体系. 现代地质, 1989, 3(3) : 267~289. [3] Ortoleva P. Geochemical Self-organization. Oxford: Oxford University Press, 1994. [4] Thompson J B Jr. Geochemical reaction and open systems. Geochim Cosmochim Acta, 1970, 34:520~551. [5] Dibble Jr W E,Tiller W A.Non-equilibrium water/rock interactions:Ⅰ.Model for interface-controlled reactions.Geochim Cosmochim Acta, 1981, 45:79~92. [6] 张荣华, Borcsik M, Crerar D. 固—液相反应体系CaF2-HCl-H2O内化学振荡的发现.科学通报, 1991, 36(20):1 836~1 837. [7] Faimon J. Oscillatory silicon and aluminum aqueous concentrations during experimental aluminosilicate weathering.Geochim Cosmochim Acta, 1996, 60:2 901~2 907. [8] 谭凯旋, 张哲儒, 王中刚. 辉铜矿溶解反应的非周期振荡. 自然科学进展, 1996, 6(6) :751~756. [9] Tan Kaixuan, Zhang Zheru, Wang Zhonggang. Chemical oscillation and chaotic attractors of dissolution reaction of chalcopyrite in NaCl solutions. Chinese Science Bullet in, 1996, 41(12): 1 020~1 023. [10] Merino E. Survey of geochemical self-patterning phenomena. In: Nicolis G, Baras F, eds. Chemical In stabilities. Boston: D Reidel Publishing Company, 1984. 305~328. [11] Haase C S,Chadam J,Feinn D,et al.Oscillatory zoning in plagioclase feldspar. Science, 1980, 209: 272~274. [12] Ortoleva P. Role of attachment kinetic feed back in the oscillatory zoning of crystals from melts. Earth Sci Rev,1990, 29: 3~8. [13] Anovitz L M. Oscillatory zonation patterns in hydrothermal grossular-andradite garnet: Nonlinear dynamics in regions of immiscibility. American Mineralogist, 1991, 76: 1 319~1 327. [14] 李如生. 岩浆岩中矿物组分分布的有序现象和耗散结构. 矿物学报,1984,4:303~310. [15] 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: 193~203. [16] 吴金平, 李才伟, 肖文丁, 等. 界面质量守恒方程和一些生长层的自组织模型. 中国科学(E辑), 1996, 26(5): 1~10. [17] 王江海, 吴金平. 硅酸盐固溶体矿物中组分的非韵律型空间分布及形成过程的动力学机制. 矿物学报, 1992, 12(1): 1~6. [18] Fowler A D. Self-organized mineral textures of igneous rocks: the fractal approach. Earth Sci Rev, 1990,29: 47~55. [19] Chadam J, Ortoleva P. Morphological instabilities in physico-chemical systems. Earth Sci Rev, 1990, 29:175~181. [20] Wollkind D J, Vislocky M. An interfacial model equation for the bifurcation of solidification patterns during LPEE processes. Earth Sci Rev, 1990, 29: 349~368. [21] Fisher G W, Lasaga A C. Irreversible thermodynamics in petrology. In: Lasaga A C, Kirkpatrick R J, eds. Kinetics of Geochemical Processes. Washington: Mineral Soc Am, 1981. 171~209. [22] Ortoleva P. The self-organization of Liesegang bands and other precipitate patterns. In: Nicolis G,Baras F,eds.Chemical Instabilities. Boston: D Reidel Publishing Company, 1984. 289~297. [23] Sultan R, Ortoleva P, DePasquale F, et al. Bifurcation of the Ostwald-Liesegang supersaturation-nucleation-depletion cycle. Earth Sci Rev, 1990,29:163~173. [24] 谭凯旋. 热水沉积中的奥斯特瓦尔德作用. 见:欧阳自远主编. 矿物岩石地球化学新探索. 北京: 地震出版社,1993. 99~101. [25] Ortol eva P,Merino E,Moore C.Geochemical self-organization Ⅰ and Ⅱ.Amer J Sci, 1987, 287:979~1 040. [26] Ripley E, Merino E, Moore C, et al. Mineral zoning in sediment-hosted copper deposits. In: Wolf K H, eds. Hand-book of Strata-Bound and Stratiform Ore Deposits, v13. Amsterdam: Elservier, 1985. 237~260. [27] 於崇文,蒋耀淞.云南个旧成矿区锡石—硫化物矿床原生金属分带形成的动力学机制.地质学报, 1990, 64 (3): 226~237. [28] Chen Wei,Ortoleva P.Reaction front fingering in carbonate-cemented sandstones.Earth Sci Rev, 1990, 29:183~198. [29] 谭凯旋, 张哲儒, 王中刚. 聚流成矿作用的非线性动力学. 矿物岩石, 1995, 15(增刊):139~140. [30] Ortoleva P, Merino E, Strickholm P. A kinetic theory of metamorphic layering in anisotropically stressed rocks.Amer J Sci, 1982, 282:617~643. [31] Dewers T,Ortoleva P.Mechano-chemical coupling in stressed rocks.Geochim Cosmochim Acta, 1989, 53:1 243~1 258. [32] Dewers T, Ortoleva P. A coupled reaction-transport-mechanical model for intergranular pressure solution, stylolites and differential compaction and cementation in clean sandstone. Geochim Cosmochim Acta, 1990, 54: 1 609~1 625. [33] Williams P F. Differentiated layering in metamorphic rocks. Earth Sci Rev, 1990, 29: 267~281. [34] Walgraef D.Reaction-transport dynamics and dissolution patterns in deformed materials. Earth Sci Rev, 1990, 29:299~308. [35] Meike A. Considerations for quantitative determination of the role of dislocations in selective dissolution. Earth Sci Rev, 1990, 29:309~320. [36] Park A, Dewers T, Ortoleva P. Cellular and oscillatory self-induced methane migration. Earth Sci Rev, 1990, 29:249~265. [37] Ghaith A, Chen Wei, Ortoleva P. Oscillatory methane release from shale source rocks. Earth Sci Rev, 1990, 29;241~248. [38] Powley D E. Pressures, hydrogeology and large scale seals in petroleum basins. Earth Sci Rev, 1990, 29:215~226. [39] Dewers T, Ortoleva P. Nonlinear dynamical as pects of deep basin hydrology: fluid compartment formation and episodic fluid release. Amer J Sci, 1994, 294:713~755. [40] Ortoleva P, Al-Shaieb Z, Puckette J. Genesis and dynamics of basin compartments and seals. Amer J Sci, 1995,295: 345~427. [41] Lasaga A C. The kinetic treatment of geochemical cycles. Geochim Cosmochim Acta, 1980, 44:815~828. [42] Cappellen P V,Wang Yifen. Cycling of iron and manganese in surface sediments: a general theory for the coupled transport and reaction of carbon, oxygen, nitrogen, sulfur, iron and manganese. Amer J Sci, 1996, 296: 197~243. |