构造体制转换与流体多层循环成矿动力学

邓军; 杨立强; 孙忠实; 彭润民; 陈学明; 杜子图

构造体制转换与流体多层循环成矿动力学

1.
中国地质大学地球科学与资源学院，北京 100083
2.
中国科学院地质与地球物理研究所，北京 10010
3.
长春科技大学，长春 130061

基金项目:

国家重点基础研究发展规划项目 G1999043206

国土资源部“百名跨世纪科技人才培养计划”基金 9808

国家攀登计划项目 95-预-25

国家攀登计划项目 95-预-39

；国土资源部“九五”重点基础项目 9501103

详细信息

作者简介:
邓军，男，1958年生，教授，博士生导师，构造地质学和矿床学专业，主要从事区域构造、成矿流体及成矿动力学的教学和科研工作

中图分类号: P611.5; P542
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- 被引次数: 0
出版历程
- 收稿日期: 2000-03-26
- 刊出日期: 2000-07-25

ORE-FORMING DYNAMICS OF TECTONIC REGIME TRANSFORMATION AND MULTI-LAYER FLUID CIRCULATION

1.
Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 10008, China
2.
Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100101, China
3.
Changchun University of Sciences and Technology, Changchun 130061, China

摘要

摘要: 基于成矿系统动力学研究进展的综合分析, 认为构造体制转换与流体多层循环成矿动力学研究是地球科学跨世纪的重要前沿领域之一, 进而提出这一领域的研究主题和关键问题、研究思路及方法, 阐释其重要意义, 指出构造体制转换与流体多层循环成矿动力学研究以构造演化、流体活动及区域地球化学和地球物理不均一性为基础, 通过变形-流动高温高压实验及计算机数值模拟再现成矿作用过程和机理, 解析构造体制转换与流体多层循环成矿动力学特征, 揭示成矿界面时-空演化规律, 建立成矿系统物质和能量交换-反馈耦合成矿的定量模型.这是深化矿床成因认识的重要基础和实现科学找矿的有效途径, 对地球系统科学和大陆动力学的研究也具有重要意义.
- 构造体制转换 /
- 流体多层循环 /
- 界面演化 /
- 成矿动力学
Abstract: The comprehensive analysis of advances in the research into the ore forming dynamics concludes in this paper that the research into the ore forming dynamics of the tectonic regime transformation and multi layer circulation is on the cutting edge of the earth sciences in the 21st century. Then the paper presents the theme, key issues, methodology, and important significance of this research. In addition, this paper also proposes that the research into the ore forming dynamics of the tectonic regime transformation and the multi layer fluid circulation centers around the heterogeneities in the structural evolution, fluid activity, regional geochemistry and geophysics. The experiments on the deformation fluid high temperature and high pressure, the method for numerical simulation to reappear the ore forming process and mechanism, to analyze the ore forming dynamics of the tectonic regime transformation and multi layer fluid circulation, to reveal tempo spatial evolutionary patterns of the ore forming interfaces, and finally to construct the quantitative model of the exchange between material and energy feedback coupling mineralization in the mineralization system. This research, an important basis of the deeper understanding of the mineralization origin, and an effective approach to the scientific mineral prospecting, is of great significance to the research into the earth system science and continental dynamics.
- tectonic regime transformation /
- multi-layer fluid circulation /
- evolution of ore-forming interface /
- mineralization dynamics

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参考文献(85)

[1]	翟裕生. 论成矿系统[J]. 地学前缘, 1999, 6 (1): 13~28. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY201405016.htm
[2]	中国地球科学发展战略研究组. 中国地球科学发展战略的若干问题———从地学大国到地学强国[J]. 地球科学进展, 1999, 14 (2): 105~109. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ902.000.htm
[3]	Ohmho H. When did the earth's atmosphere becomeoxic[J]? Newsletter of Geochemical Society, 1997, 93: 26~27.
[4]	翟裕生. 地史中成矿演化的趋势和阶段性[J]. 地学前缘, 1997, 4 (3-4): 197~203. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY7Z2.034.htm
[5]	Barley M E, Groves D I. Supercontinent cycles and the distribution of metal deposits through time[J]. Geology, 1992, 20: 291~294.
[6]	郭文魁. 论成矿作用在构造-岩浆活动中的地球化学演化特征[J]. 地学研究, 1997, (29~30): 1~7. https://cpfd.cnki.com.cn/Article/CPFDTOTAL-ZGDJ199700001005.htm
[7]	Doe B R, Zartman R E. Plume bottom tectonics, the Phanerozoic [A]. In: Barnes H L, ed. Geochemistry of hydrothermal ore deposits[C]. 2nd ed. [s. l. ]: John Wiley & Sons, 1979.22~79.
[8]	Детников Ф А. К проблеме вертикально й зональности и рудоносности глубинных разломов докембрия [J ]. Геология рудных месторождений, 1991, (2): 15~24.
[9]	顾连兴, 何金祥, 胡文喧, 等. 陆壳成熟度对于华南块状硫化物矿床的成分效应[J]. 地质科学, 1997, 71 (2): 161~169. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE199702007.htm
[10]	Groves D I. Archean lode-gold deposits: the products of crust-scale hydrothermal systems[J]. Brazil Gold, 1991, 9l: 299~305.
[11]	涂光炽. 超大型矿床的探寻与研究的若干问题[J]. 地学前缘, 1994, 1 (3): 45~52.
[12]	Hutchison C S. Economic deposits and their tectonic setting[M]. NewYork: Macmillan, 1994.1~391.
[13]	Zhai Y S, Deng J. An outline of mineral resources of China and their tectonic setting[J]. Australian Journal of Earth Sciences, 1996, 43: 673~685. doi: 10.1080/08120099608728286
[14]	裴荣富. 金属成矿省地质历史演化与特大型矿床[J]. 矿床地质, 1997, 16 (2): 169~170. https://www.cnki.com.cn/Article/CJFDTOTAL-KCDZ702.007.htm
[15]	Kutina J. The role of mantle-rooted structural discontinuities in concentration of metals[J]. Global Tectonics and Metallogeny, 1996, 5: 79~102. doi: 10.1127/gtm/5/1996/79
[16]	涂光炽. 九十年代固体地球科学及超大型矿床研究若干进展[J]. 矿物学报, 1997, 17 (4): 357~363. https://www.cnki.com.cn/Article/CJFDTOTAL-KWXB199704000.htm
[17]	翟裕生, 张湖, 宋鸿林, 等. 大型构造与超大型矿床[M]. 北京: 地质出版社, 1997.1~180.
[18]	Houseman G A, McKenzie D P, Molnar P. Convergent in stability of thickened boundary layer and its relevance for the thermal evolution of convergent belts[J]. Journal of Geophysics Review, 1981, 86: 6135~6155.
[19]	Fyfe W S, Price N J, Thompson A B. Fluids in the Earth'scrust[M]. Amsterdam, Oxford, NewYork: Elserier Scientific Publishing Company, 1978.1~383.
[20]	Meissner K, Wever R. The possible role of fluids for the structuring of the continental crust[J]. Earth Science Reviews, 1992, 32: 19~32. doi: 10.1016/0012-8252(92)90010-Q
[21]	Newton R C. Fluids and shear zones in the deepcrust[J]. Tectonophysics, 1990, 182: 21~27. doi: 10.1016/0040-1951(90)90339-A
[22]	Newton R C. 深部地壳中的变质流体[J]. 许碧燕, 译. 国外地质科技, 1990, 8: 1~90.
[23]	卢焕章. 成矿流体[M]. 北京: 科学技术出版社, 1997.1~207.
[24]	贾跃明. 流体成矿系统与成矿作用研究[J]. 地学前缘, 1996, 3 (4): 253~258. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY604.012.htm
[25]	张文淮, 张志坚, 伍刚. 成矿流体及成矿机制[J]. 地学前缘, 1996, 3 (4): 245~252. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY604.011.htm
[26]	Deutsh A. Isotope systematic support the impact origin of the Sudbury structure (Ontario, Canada)[J]. Geological Society of America, 1997, 293 (Special Paper): 6~11.
[27]	傅昭仁, 李紫金. 对加拿大萨德伯里撞击构造的考察及其启示[J]. 地质科技情报, 1996, 15 (4): 57~64. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ604.013.htm
[28]	Krogh T E, Davis D W, Crofu F. Precise U-Pb zircon and baddeleyite ages for the Sudbury area[J]. The Geology and Ore Deposits of the Sudbury Structure, 1984, 1 (OGSS pecial): 431~447.
[29]	Cox S F, Wall V J, Etheridge M A, et al. Deformational and metamorphic processes in the formation of mesothemal vein-hosted gold deposits—example from the Lach-lan fold in central Victoria[J]. Ore Geol Rev, 1991, 6: 391~423. doi: 10.1016/0169-1368(91)90038-9
[30]	Benning L G, Seward T M. Hydrosuphide complexing of gold (I) in hydrothermal solution from 150℃ to 500℃ and 500to 15 00 bars[J]. Geochim Cosmochim Acta, 1996, 60: 1849~1877. doi: 10.1016/0016-7037(96)00061-0
[31]	Bower T S. The deposition of gold and other metals: pressure induced fluid immiscibility and associated stable isotope signatures[J]. Geochim Cosmochim Acta, 1991, 55: 2447~2434.
[32]	张荣华, 胡书敏. 含矿热液系统的化学动力学研究若干基本问题[J]. 矿床地质, 1998, 17 (增刊): 1035~1038.
[33]	Matthai S K, Henely R W, Heinrich C A. Gold precipi-tation by fluid mixing in bedding-parallel fractures near Carbonaceous slates at the Cosmopolitan Howley gold deposit, Northern Australia[J]. Economic Geology, 1995, 90: 2123~2142. doi: 10.2113/gsecongeo.90.8.2123
[34]	Cline J S, Bondnar R J, Rimstidt J D. Numerical simulation of fluid flow and silica transport and deposition in boiling hydrothermal solutions: application to epithermal gold deposits[J]. Journal Geophysics Review, 1992, 97: 9085~9103. doi: 10.1029/91JB03129
[35]	Reed M H. Computer modeling of chemical processed in geothermal systems: examples of water-rock reaction, boiling and mixing [A]. In: Damore F, ed. Applications of geochemistry in geothermal reservoir development[C]. NewYork: Inst for Training and Research, 1992.275~298.
[36]	洛斯ВЛ. 热液成矿作用的计算模拟[J]. 地质科技动态, 1997, (2): 14~15.
[37]	Haynes D W. Olympic dam ore genesis: a fluid-mixing model[J]. Economic Geology, 1995, 90: 281. doi: 10.2113/gsecongeo.90.2.281
[38]	Bonnemaison M. "Filons de aurifere" an cas particulier de shear aurifere[J]. Chron Rech Min, 1986, 482: 55~66.
[39]	Miller A R. High salinity in sea water[J]. Nature, 1964, 203: 590~594. doi: 10.1038/203590a0
[40]	Shanks W C Ⅲ, Bischoff L. Geochemistry, sulfur isotope composition, and accumulation rates of red sea geothermal deposits[J]. Economic Geology, 1980, 75: 445~459. doi: 10.2113/gsecongeo.75.3.445
[41]	池三川. 现代成矿理论的某些进展[J]. 地学前缘, 1994, 1 (3): 83~88. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY403.009.htm
[42]	翟裕生. 矿床地质学的发展前景和思维方法[J]. 地学前缘, 1994, 1 (3): 1~8. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY403.000.htm
[43]	银剑钊. 纳米矿床学[J]. 地学前缘, 1994, 1(3): 8. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY403.001.htm
[44]	Cox S F. Faulting processes at high fluid pressures: an example of fault valve behavior from the Wattle Gully fault, Victoria, Australia[J]. Journal of Geophysical Research(B), 1995, 100 (7): 13007~13020.
[45]	Houseman G. From mountains to basin[J]. Nature, 1996, 379: 771~772. doi: 10.1038/379771a0
[46]	Seber D, Barazangi M, Ibebrahim, et al. Geophysical evidence for lithospheric delimitation beneath the Alboran Sea and Rif-Betic mountains[J]. Nature, 1996, 379: 785~790. doi: 10.1038/379785a0
[47]	Quick J E. Emplacement dynamics of a large mantle intrusionin the lower crust, Ivren-verbano zone, Northern Italy[J]. Journal Geophysics Review, 1994, 99(B11): 21559~21573. doi: 10.1029/94JB00113
[48]	Caress D W. Seismic imaging of hotspot-related crustal underplating beneath the Marquesas island[J]. Nature, 1995, 373: 600~603. doi: 10.1038/373600a0
[49]	Liu M. Intrusion and underplating of mafic magma; ther-mal-geological effect and implications for Tertiary tectono-magmatism in the North American Cordillera[J]. Tectonophysics, 1994, 237(3): 175~187.
[50]	邓万明, 丁大赉. 壳-幔过渡带及其在岩石圈构造演化中的地质意义[J]. 科学通报, 1997, 42(23): 2474~2482. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB199723001.htm
[51]	金振民, 白武明. 动态部分熔融作用及其地球物理意义[J]. 地质科技情报, 1993, 12(1): 1~7. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ199301022.htm
[52]	Hill R I, Campoell I H, Davies G F, et al. Mantle plumes and continental tectonics[J]. Sciences, 1992, 256: 186~193. doi: 10.1126/science.256.5054.186
[53]	National Research Council. Solid-earth sciences and society[M]. Washington D C: National Academy Press, 1993.
[54]	滕吉文. 跨世纪的地学盛会———第31届世界地质大会[J]. 科学, 1997, (3): 1~6.
[55]	Olson P, Nam I S. Formation of seafloor swells by mantle plumes[J]. Journal of Goephysics Review, 1986, 91: 7181~7191.
[56]	孙岩, 刘海龄. 浅层构造反转体制中的两个水岩反应系列[J]. 南京大学学报, 1997, 33 (地质流体专辑): 53~59.
[57]	Goddard J V, Evans J P. Chemical change and fluid-rock interaction in fault of crystalline thrust sheets, northwestern Wyoming, USA[J]. Journal Structure Geology, 1995, 17: 553~547.
[58]	Richard H S, Francois R K. High-angle reverse faults fluid pressure cycling, and mesothermal gold quartz deposits[J]. Geology, 1988, 16: 551~555.
[59]	David C E, Arne B, Tom A. Fluid evolution and Au-Cu genesis along a shear zone: a regional fluid inclusion study of shear zone hosted alteration and gold and copper miner-alization in the Kautokeino greenstone belt, Finnmark Norway[J]. Journal of Geochemical Exploration, 1993, 49: 233~267. doi: 10.1016/0375-6742(93)90047-P
[60]	Eion M. Cameron derivation of gold by oxidative metamorphism of a deep ductile shear zones(part 2): evidence from the Bamble Belt, South Norway[J]. Journal of Geochemical Exploration, 1989, 31: 149~169. doi: 10.1016/0375-6742(89)90004-6
[61]	Jiang Z W, Oliver N H S, Barr T D, et al. Numerical modeling of fault-control led fluid flow in the genesis of tin deposits of the Malage ore field, Gejiu mining district, China[J]. Economic Geology, 1997, 86: 228~247.
[62]	Dirks P H, Wilson C J. Structural controls on the distri bution of gold-bearing quartz vein in the Arltunga gold field, Northern Territory, Australia[J]. Economic Geology, 1991, 86: 249~269. doi: 10.2113/gsecongeo.86.2.249
[63]	Reinhardt M C, Davison I. Structural and lithologic controls on gold deposition in the shear zone-hosted Fazenda Brasileiro Mine, Bahia State, Northern Brazil[J]. Economic Geology, 1990, 85: 952~967. doi: 10.2113/gsecongeo.85.5.952
[64]	邓军, 吕古贤, 杨立强, 等. 构造应力场转换与界面成矿[J]. 地球学报, 1998, 19(3): 244~250. https://www.cnki.com.cn/Article/CJFDTOTAL-DQXB803.003.htm
[65]	邓军, 翟裕生, 杨立强, 等. 剪切带构造-流体-成矿系统动力学模拟[J]. 地学前缘, 1999, 6(1): 115~127. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY901.015.htm
[66]	Barton C C. Fractal analysis of scaling and spatial clustering of fractures [A]. In: Barton C C, ed. Fractals in the earth sciences[C]. NewYork: Plenum Press, 1995.54~67.
[67]	Zhang X, Sanderson D J. Fractal structure and deformation of fractured rock masses [A]. In: Kruhl J H, ed. Fractal and dynamical systems in geosciences[C]. Berlin, Heidelberg: Springer-Verlag, 1994.37~51.
[68]	邓军, 杨立强, 方云, 等. 成矿系统嵌套分形结构和自有序效应[J]. 地学前缘, 2000, 7(1~2): 133~146. https://www.cnki.com.cn/Article/CJFDTOTAL-DXQY200001017.htm
[69]	Rumble D, Yui T F. The Qinglongshan oxygen and hydrogen isotope anomaly near Donghai in Jiangsu Province, China[J]. Geochim Cosmochim Acta, 1999, 62: 3307~3321.
[70]	Sverjensky D A, Garven G. Tracing great fluid migrations[J]. Nature, 1992, 356: 481~511. doi: 10.1038/356481a0
[71]	Young E D. Fluid flow in metamorphic environments[J]. Rev Geophys, 1995, 33 (Suppl): 41~52.
[72]	Ferry J M. A historical review of metamorphic fluid flow[J]. J Geophys Res, 1994, 99B: 15487~15498.
[73]	Oliver N H S. Review and classification of structural controls on fluid flow during regional metamorphism[J]. J Metamor Geol, 1996, 14: 477~492. doi: 10.1046/j.1525-1314.1996.00347.x
[74]	Oliver J. Fluids expelled tectonically from organic belts: their role in hydrocarbon migration and other geologic phenomena[J]. Geology, 1986, 18: 99~102.
[75]	Bjorkum P A. Fluid flow in sedimentary basins[J]. Sedi mentary Geology, 1993, 86: 137~158. doi: 10.1016/0037-0738(93)90137-T
[76]	Bethke C M, Reed J D, Oltz D F. Long-range petroleum migration in the Illinois Basin[J]. AAPG Bull, 1991, 75: 925~945.
[77]	Garven G, Freeze R A. Theoretical analysis of the role of groundwater flow in the genesis of stratabound ore deposits 2, Quantitative results[J]. American Journal Sciences, 1984, 284: 1125~1174.
[78]	Screaton E J. Permeabilities, fluid pressure, and flow rates in the Barbados Ridge complex[J]. Journal of Geophysical Research, 1990, 95: 8997~9007. doi: 10.1029/JB095iB06p08997
[79]	Tobin H J. Fluid pressures in the frontal thrust of the oregon accretionary prism: experimental constrains[J]. Geology, 1994, 22: 979~982.
[80]	Fisher A T. Relation between permeability and effective stress along a plate-boundary complex[J]. Geology, 1996, 24: 307~310.
[81]	RockN M S, Grovs D I. Can lamprophyres resolve the genetic controversy over mesothermal gold deposits[J]?Geology, 1988, 16: 5 38~541.
[82]	Navon O. Mantel-drived fluids in diamond micro-inclusions[J]. Nature, 1988, 335: 784~789. doi: 10.1038/335784a0
[83]	季克俭, 吴学汉, 张国炳. 热液矿床的矿源、水源和热源及矿床分布规律[M]. 北京: 科学技术出版社, 1991.1~130.
[84]	Faber E. Origin of hydrocarbon gases in the pump-test of the KTB pilot well[J]. Scientific Drilling, 1995, (5): 123~28.
[85]	Richard A Kerr. German super-deep hole hits bottom[J]. Science, 1994, 266 (28): 545.