[1]Dickens G R. Rethinking the global carbon cycle with a large, dynamic and microbially mediated gas hydrate capacitor[J]. Earth and Planetary Science Letters,2003, 213: 169-183. [2]Chen D F, Su Z, Cathles L M. Types of gas hydrates in marine environments and their thermodynamic characteristics [J]. Terrestrial, Atmospheric and Oceanic Sciences,2006,17:723-737. [3]Chen Zhong,Yan Wen,Chen Muhong, et al. Advances in gas hydrate dissociation and fate of methane in marine sediment [J]. Advances in Earth Science, 2006, 21(4):394-400. [陈忠,颜文,陈木宏,等. 海底天然气水合物分解与甲烷归宿研究进展[J].地球科学进展,2006,21(4):394-400.] [4]Yu Xiaoguo, Li Jiabiao. Advance in gas hydrate dissociation and effects on the ecology and environment[J]. Advances in Earth Science, 2004,19(6): 947-954. [于晓果,李家彪.天然气水合物分解及其生态环境效应研究进展[J].地球科学进展,2004,19(6): 947-954.] [5]Castellini D G, Dickens G R , Snyder G T, et al. Barium cycling in shallow sediment above active mud volcanoes in the Gulf of Mexico [J]. Chemical Geology, 2006, 226: 1-30. [6]Torres M E, Brumsack H J, Bohrmann G, et al. Barite fronts in continental margin sediments: A new look at barium remobilization in the zone of sulfate reduction and formation of heavy barites in diagenetic fronts [J]. Chemical Geology, 1996, 127: 125-139. [7]Torres M E, McManus J, Huh C A. Fluid seepage along the San Clemente Fault scarp: Basin-wide impact on barium cycling [J]. Earth and Planetary Science Letters, 2002, 203: 181-194. [8]Dickens G R, Fewless T, Thomas E, et al. Excess barite accumulation during the Paleocene Eocene thermal maximum: massive input of dissolved barium from seafloor gas hydrate reservoirs[C]//Wing S L, Gingerich P D, Schmitz B, eds. Causes and Consequences of Globally Warm Climates in the Early Paleogene. Special Paper, Geological Society of America, 2003,369: 11-23. [9]Feng Dong, Chen Duofu, Su Zheng, et al. Advances on the anaerobic methane oxidation and seep carbonates precipitation kinetics at seafloor [J]. Marine Geology and Quaternary Geology, 2006, 26(3):125-131. [冯东,陈多福,苏正,等. 海底甲烷缺氧氧化与冷泉碳酸盐岩沉淀动力学研究进展[J].海洋地质与第四纪地质,2006,26(3):125-131.] [10]Dickens G R. Sulfate profiles and barium fronts in sediment on the Blake Ridge: present and past methane fluxes through a large gas hydrate reservoir [J]. Geochimica et Cosmochimica Acta,2001, 65: 529-543. [11]Riedinger N, Kasten S, Gröger J, et al. Active and bruied authigenic barite fronts in sediments from the Eastern Cape basin[J]. Earth and Planetary Science Letters,2006, 241: 876-887. [12]Aloisi G, Wallmann K, Bollwerk S M, et al. The effect of dissolved barium on biogeochemical processes at cold seeps [J]. Geochimica et Cosmochimica Acta, 2004, 68, 1735-1748. [13]Torres M E, Bohrmann G, Dubé, T E,et al. Formation of modern and Paleozoic stratiform barite at cold methane seeps on continental margins [J]. Geology,2003, 31, 897-900. [14]Davie M K, Buffett B A. A numerical model for the formation of gas hydrate below the seafloor [J]. Journal of Geophysical Research, 2001, 106: 497-514. [15]Cathles L M, Chen D F. A compositional kinetic model of hydrate crystallization and dissolution [J]. Journal of Geophysics Research,2004, 109, B08102, doi:10.1029/2003JB002910. [16]Chen Duofu, Feng Dong, Cathles L M. Kinetics of gas hydrate reservoir formation and gas potential assessment in the marine gas vent system[J]. Geotectonica et Metallogenia,2005, 29(2): 278-284. [陈多福,冯东, Cathles L M.海底天然气渗漏系统水合物成藏动力学及其资源评价方法[J].大地构造与成矿学,2005,29(2): 278-284.] [17]Luff R, Wallmann K. Fluid flow, methane fluxes, carbonate precipitation and biogeochemical turnover in gas hydrate-bearing sediments at hydrate ridge, Cascadia margin numerical modeling and mass balances [J]. Geochimica et Cosmochimica Acta,2003,67:3 403-3 421. [18]Suess E, Torres M E, Bohrmann G, et al. Gas hydrate destabilization: Enhanced dewatering, benthic material turnover, and large methane plumes at the Cascadia Margin [J]. Earth and Planetary Science Letters,1999, 170: 1-15. [19]Dymond J, Suess E, Lyle M. Barium in deep-sea sediments: A geochemcial proxy for paleoproductivity [J]. Paleoceanography,1992, 7: 163-181. [20]Gingele F, Dahmke A. Discrete barite particles and barium as tracers of paleoproductivity in South Atlantic sediments [J]. Paleoceanography,1994, 9: 151-168. [21]Von Breymann M T, Emeis K C, Camerlenghi A. Geochemistry of sediments from the Peru upwelling area: Results from Sites 680, 682, 685 and 688[C]//Suess E, eds. Proceedings of the Ocean Drilling Program, Scientific Results. Texas A & M University, College Station, Texas, USA, 1990, 112: 491-503. [22]Von Breymann M T, Brumsack H, Emeis K -C. Deposition and diagenetic behavior of barium in the Japan sea[C]//Sciotto K A, eds. Proceedings of the Ocean Drilling Program, Scientific Results. Texas A & M University, College Station, Texas, USA, 1992,127/128: 651-665. [23]Monnin C. A thermodynamic model for the solubility of barite and celestite in electrolyte solutions and seawater to 200℃ and to 1 kbar [J]. Chemical Geology,1999, 153: 187-209. [24]McManus J, Berelson W M, Klinkhammer G P, et al. Geochemistry of barium in marine sediments: Implications for its use as a paleoproxy[J]. Geochimica et Cosmochimica Acta,1998, 62:3 453-3 473. [25]Fu B, Aharon P. Sources of hydrocarbon-rich fluids advecting on the seafloor in the northern Gulf of Mexico[C]//Transactions Gulf Coast Association of Geological Societies.1998, 48: 73-81. [26]Naehr T H, Stakes D S, Moore W S. Mass wasting, ephemeral fluid flow and barite deposition on the California continental margin [J]. Geology,2000, 28: 315-318. [27]Campbell K A. Hydrocarbon seep and hydrothermal vent paleoenvironments and paleontology: Past developments and future research directions [J]. Palaeogeography, Palaeoclimatology, Palaeoecology,2006, 232: 362-407. [28]Borowski W S, Paull C K, Ussler W III. Marine pore water sulfate profiles indicate in situ methane flux from underlying gas hydrate [J]. Geology,1996, 24: 655-658. [29]Borowski W S, Paull C K, Ussler W III. Global and local variations of interstitial sulfate gradients in deep-water, continental margin sediments: Sensitivity to underlying methane and gas hydrates [J]. Marine Geology,1999, 159: 131-154. [30]Suess E, Bohrmann G, Von Huene R, et al. Fluid venting in the eastern Aleutian subduction zone [J]. Journal of Geophysics Research,1998,103:2 597-2 614. [31]Torres M E, Bohrmann G, Suess E. Authigenic barites and fluxes of barium associated with fluid seeps in the Peru subduction zone [J]. Earth and Planetary Science Letters,1996, 144: 469-481. [32]Fu B, Aharon P, Byerly G R, et al. Barite chimneys of the Gulf of Mexico slope: Initial report on their petrography and geochemistry [J]. Geo-Marine Letters,1994, 14: 81-87. [33]Greinert J, Boolwerk S M, Derkachev A, et al. Massive barite deposits and carbonate mineralization in the Derugin Basin, Sea of Okhotak: Precipitation processes at cold seep sites [J]. Earth and Planetary Science Letters,2002, 203: 165-180. [34]Berner R A. Diageenetic models of dissolved species in the interstitial waters of compacting sediments [J]. American Journal of Sciences,1975, 275: 88-96. [35]Li Y, Gregory S. Diffusion of ions in sea water and in deep-sea sediments [J]. Geochimica et Cosmochimica Acta,1974, 38: 703-714. [36]Iversen N, J rgensen B B. Diffusion coefficients of sulfate and methane in marine sediments: Influence of porosity [J]. Geochimica et Cosmochimica Acta,1993, 57: 571-578. [37]Niew hner C, Hensen C, Kasten S, et al. Deep sulfate reduction completely mediated by anaerobic methane oxidation in sediments of the upwelling area off Namibia[J]. Geochimica et Cosmochimica Acta, 1998, 62: 455-464. [38]Hoffman P F, Schrag D P. The snowball Earth hypothesis: Testing the limits of global change [J]. Terra Nova,2002, 14: 129-155. [39]Jiang G, Kennedy M J, Christie-Blick N. Stable isotopic evidence for methane seeps in Neoproterozoic postglacial cap carbonates [J]. Nature,2003, 426: 822-826. [40]Wang Jiasheng,Gan Huayang,Wei Qing, et al. Stable isotopes of carbon and sulfur of cap dolomite in the Three Gores and its mechanism discussion[J]. Geoscience,2005,19(1):14-20. [王家生,甘华阳,魏清,等.三峡“盖帽”白云岩的碳、硫稳定同位素研究及其成因探讨[J].现代地质,2005,19(1): 14-20.] [41]Ramkumar M, Harting M, Stüben D. Barium anomaly preceding K/T boundary: possible causes and implications on end Cretaceous events of K/T sections in Cauvery basin (India), Israel, NE-Mexico and Guatemala [J]. International Journal of Earth Sciences,2005, 94: 475-489. [42]Lü Zhicheng, Liu Congqiang, Liu Jiajun, et al. The bio-barite in witherite deposits from Southern Qinling and its significance [J]. Progress in Natural Science,2004, 14(8): 892-897.[吕志成,刘丛强,刘家军,等.南秦岭毒重石成矿带矿床中的生物成因重晶石及其意义[J].自然科学进展,2004,14(8): 892-897.] [43]Koski R A, Lonsdale P F, Shanks W C, et al. Mineralogy and geochemistry of a sediment hosted hydrothermal sulfide deposit from the southern trough of the Guaymas basin, Gulf of California [J]. Journal of Geophysical Research,1985,90:6 695-6 707. [44]Paytan A, Kastner M, Martin E E, et al. Marine barite as a monitor of seawater strontium isotope composition[J]. Nature, 1993, 366: 445-449. [45]Paytan A, Mearon S, Cobb K, et al. Origin of marine barite deposits: Sr and S isotope characterization [J]. Geology, 2002, 30: 747-750. [46]Aquilina L, Bourgois J, Fouillac A M, et al. Massive barite deposits in the convergent margin off Peru: Implications for fluid circulation within subduction zones [J]. Geochimica et Cosmochimica Acta, 1997, 61: 1 233-1 245. [47]Shikazono N. Precipitation mechanisms of barite in sulfate-sulfide deposits in back-arc basins [J]. Geochimica et Cosmochimoca Acta, 1994,58:2 203-2 213. [48]Wang Z, Li G. Barite and witherite deposits in Lower Cambrian shales of South China:Stratigraphic distribution and geochemical characterization[J]. Economic Geology,1991, 86: 354-363. [49]Paytan A, Kastner M, Campbell D, et al. Sulfur isotopic composition of Cenozoicseawater sulfate [J].Science,1998,282:1 459-1 462. |