用户名: 密码: 验证码:
Seafloor hydrothermal activity and polymetallic sulfide exploration on the southwest Indian ridge
详细信息    查看全文
  • 作者:Chunhui Tao (1)
    Huaiming Li (1)
    Xiaobing Jin (1)
    Jianping Zhou (1) (2)
    Tao Wu (1)
    Yonghua He (1)
    Xianming Deng (1)
    Chunhua Gu (1)
    Guoyin Zhang (1)
    Weiyong Liu (1)
  • 关键词:Ultraslow spreading ridge ; Southwest Indian ridge ; Seafloor hydrothermal activity ; Polymetallic sulfide ; Chinese cruise
  • 刊名:Chinese Science Bulletin
  • 出版年:2014
  • 出版时间:July 2014
  • 年:2014
  • 卷:59
  • 期:19
  • 页码:2266-2276
  • 全文大小:
  • 参考文献:1. Herzig P, Hannington MD, Petersen S (2002) Polymetallic massive sulphide deposits at the modern seafloor and their resources potential. In: International Seabed Authority technical study 2, report on the UN workshop on seafloor mineral resources, 2000, Kingston, Jamaica, pp 8-5
    2. Zierenberg RA, Fouquet Y, Miller DJ et al (1998) The deep structure of a sea-floor hydrothermal deposit. Nature 392:485-88 CrossRef
    3. Baker ET, German CR (2004) On the global distribution of hydrothermal vent fields. In: German CR, Lin J, Parson LM et al (eds) Mid-ocean ridges: hydrothermal interactions between the lithosphere and oceans. AGU geophysical monograph series. Wiley, Washington, DC, pp 245-66
    4. Hannington M, Jamieson J, Monecke T et al (2011) The abundance of seafloor massive sulfide deposits. Geology 39:1155-158 CrossRef
    5. Ian L (2012) Mineral resource estimated Solwara Project. Bismarck Sea, Papua New Guinea
    6. SRK Consulting Pty Ltd (2012) NI 43-101 technical report 2011 PNG, Tonga, Fiji, Solomon Island, New Zealand, Vanuatu and the ISA
    7. Alt JC (2003) Hydrothermal fluxes at mid-ocean ridges and on ridge flanks. CR Geosci 335:853-64 CrossRef
    8. Stein CA, Stein S (1994) Constrains on hydrothermal heat flux through the oceanic lithosphere from the global heat flow. J Geophys Res 99:3081-196 CrossRef
    9. Tivey MK (2007) Generation of seafloor hydrothermal vent fluids and associated mineral deposits. Oceanography 20:50-5 CrossRef
    10. Van Dover C (2000) The ecology of deep-sea hydrothermal vents. Princeton University Press, Princeton
    11. Martin W, Baross J, Kelley D et al (2008) Hydrothermal vents and the origin of life. Nat Rev Microbiol 6:805-14
    12. German CR, Lin J (2004) The thermal structure of the oceanic crust, ridge-spreading and hydrothermal circulation: how well do we understand their inter-connections? In: German CR, Lin J, Parson LM et al (eds) Mid-ocean ridges: hydrothermal interactions between the lithosphere and oceans. AGU geophysical monograph series. Wiley, Washington, DC, pp 1-8 CrossRef
    13. Tao C, Lin J, Guo S et al (2012) First active hydrothermal vents on an ultraslow-spreading center: southwest Indian Ridge. Geology 40:47-0 CrossRef
    14. Tao CH, Wu GH, Ni JY et al (2009) New hydrothermal fields found along the SWIR during the Legs 5- of the Chinese DY115-20 expedition. In: American Geophysical Union, Fall Meeting 2009, abstract OS21A-1150
    15. Tao CH, Lin J, Guo SQ et al (2007) The Chinese DY115-19 Cruise: discovery of the first active hydrothermal field at the ultraslow spreading Southwest Indian Ridge. InterRidge News 16:25-6
    16. Han X, Wu G, Cui R et al (2010) Discovery of a hydrothermal sulfide deposit on the Southwest Indian Ridge at 49.2°E. In: American Geophysical Union, Fall Meeting 2010, abstract OS21C-1531
    17. Sauter D, Cannat M, Meyzen C et al (2009) Propagation of a melting anomaly along the ultraslow Southwest Indian Ridge between 46°E and 52°20′E: interaction with the Crozet hotspot? Geophys J Int 179:687-99 CrossRef
    18. Zhang T, Lin J, Gao JY (2011) Interactions between hotspots and the Southwest Indian Ridge during the last 90?Ma: implications on the formation of oceanic plateaus and intra-plate seamounts. Sci China Earth Sci 254:1177-188 CrossRef
    19. Georgen JE, Lin J, Dick HJB (2001) Evidence from gravity anomalies for interactions of the Marion and Bouvet hotspots with the Southwest Indian Ridge: effects of transform offsets. Earth Planet Sci Lett 187:283-00 CrossRef
    20. Chen YJ, Morgan JP (1996) The effect of magma emplacement geometry, spreading rate, and crustal thickness on hydrothermal heat flux at mid-ocean ridge axes. J Geophys Res 101:475-82
    21. Chen YJ, Lin J (1999) Mechanisms for the formation of ridge-axis topography at slow-spreading ridges: a lithospheric-plate flexural model. Geophys J Int 136:8-8 CrossRef
    22. Dick HJB, Lin J, Schouten H (2003) An ultraslow-spreading class of ocean ridge. Nature 426:405-12 CrossRef
    23. Dyment J, Lin J, Baker ET (2007) Ridge–hotspot interaction. Oceanography 20:102-15 CrossRef
    24. Horner-Johnson BC, Gordon RG, Cowles SM et al (2005) The angular velocity of Nubia relative to Somalia and the location of the Nubia–Somalia–Antarctica triple junction. Geophys J Int 162:221-38 CrossRef
    25. Sauter D, Carton H, Meyzen C et al (2004) Ridge segmentation and the magnetic structure of the Southwest Indian Ridge (at 50°300′E, 55°300′E and 66°200′E): implications for magmatic processes at ultraslow-spreading centers. Geochem Geophys Geosyst 5:1-5
    26. Muller MR, Minshull TA, White RS (1999) Segmentation and melt supply at the Southwest Indian Ridge. Geology 27:867-70 CrossRef
    27. Sauter D, Mendel V, Rommevaux-Jestin C et al (2004) Focused magmatism versus amagmatic spreading along the ultra-slow spreading Southwest Indian Ridge: evidence from TOBI side scan sonar imagery. Geochem Geophys Geosyst 5:1-0
    28. Cannat M, Rommevaux-Jestin C, Sauter D et al (1999) Formation of the axial relief at the very slow spreading Southwest Indian Ridge (49°E-9°E). J Geophysil Res 104:22825-2843 CrossRef
    29. Meyzen CM, Toplis MJ, Humler E et al (2003) A discontinuity in mantle composition beneath the southwest Indian Ridge. Nature 421:731-33 CrossRef
    30. Seyler M, Cannat M, Mével C (2003) Evidence for major-element heterogeneity in the mantle source of abyssal peridotites from the Southwest Indian Ridge (52°E-9°E). Geochem Geophys Geosyst 4:1-3 CrossRef
    31. Font L, Murton BJ, Roberts S et al (2007) Variations in melt productivity and melting conditions along SWIR (70°E-9°E): evidence from olivine-hosted and plagioclase-hosted melt inclusions. J Petrol 48:1471-494 CrossRef
    32. Sauter D, Patriat P, Rommevaux-Jestin C et al (2001) The Southwest Indian Ridge between 49°15′E and 57°E: focused accretion and magma redistribution. Earth Planet Sci Lett 192:303-17 CrossRef
    33. Georgen JE, Kurz MD, Henry JB et al (2003) Low 3He/4He ratios in basalt glasses from the western Southwest Indian Ridge (10°E-4°E). Earth Planet Sci Lett 206:509-28 CrossRef
    34. Tao CH, Li HM, Huang W et al (2011) Mineralogical and geochemical features of sulfide chimneys from the 49°39′E hydrothermal field on the Southwest Indian Ridge and their geological inferences. Chin Sci Bull 56:2828-838 CrossRef
    35. Fouquet Y, Pierre C, Etoubleau J et al (2010) Geodiversity of hydrothermal processes along the Mid-Atlantic Ridge and Ultramafic-hosted mineralization: a new type of oceanic Cu–Zn–Co–Au volcanogeic massive sulfide deposit. In: Rona PA, Devey CW, Murton BJ (eds) Diversity of hydrothermal systems on slow spreading ocean ridge. AGU geophysical monograph series. Wiley, Washington, DC, pp 321-67 CrossRef
    36. MacCaig AM, Cliff RA, Escartin JE et al (2007) Oceanic detachment faults focus very large volumes of black smoker fluids. Geology 35:935-38 CrossRef
    37. Zhang T, Lin J, Gao JY (2013) Magmatism and tectonic processes in Area A hydrothermal vent on the Southwest Indian Ridge. Sci China Earth Sci 56:2186-197 CrossRef
    38. Zhu J, Lin J, Chen YS et al (2010) A reduced crustal magnetization zone near the first observed active hydrothermal field on the Southwest Indian Ridge. Geophys Res Lett 37:L18303 CrossRef
    39. Ye J, Shi XF, Yang YM et al (2011) Mineralogy of sulfides from ultraslow spreading Southwest Indian Ridge at 49.6°E hydrothermal field and its metallogenic significance. Acta Miner Sin 31:17-9 (in Chinese)
    40. Herzig PM, Beeker KP, Stoffers P et al (1988) Hydrothermal silica chimney fields in the Galapagos spreading center at 86°W. Earth Planet Sci Lett 89:261-72 CrossRef
    41. Halbach M, Halbach P, Lüders V (2002) Sulfide-impregnated and pure silica precipitates of hydrothermal origin from the Center Indian Ocean. Chem Geol 182:357-75 CrossRef
    42. Stüben D, Taibi NE, McMurtry GM et al (1994) Growth history of a hydrothermal silica chimney from the Mariana backarc spreading center. Chem Geol 113:273-96 CrossRef
    43. Knott R, Fouquet Y, Honnorez Y et al (1998) Petrology of hydrothermal mineralization: a vertical section through the TAG mound. Proc ODP Sci Results 158:5-6
    44. Sun ZL, Zhou HY, Yang QH et al (2012) Construction of modern low-temperature and Si-rich chimneys: with CDE hydrothermal field in Lau Basin as an example. Sci China Earth Sci 42:1544-558 (in Chinese)
    45. Peng XT, Chen S, Zhou HY et al (2011) Diversity of biogenic minerals in low-temperature Si-rich deposits from a newly discovered hydrothermal field on the ultraslow spreading Southwest Indian Ridge. J Geophys Res 116:1-8
    46. Bradley AS, Hayes JM, Summons RE (2008) Extraordinary 13C enrichment of diether lipids at the Lost City hydrothermal field indicates a carbon-limited ecosystem. Geochim Cosmochim Acta 73:102-18 CrossRef
    47. Brazelton WJ, Schrenk MO, Kelley DS et al (2006) Methane- and sulfur-metabolizing microbial communities dominate the Lost City hydrothermal field ecosystem. Appl Environ Microbiol 72:6257-270 CrossRef
    48. Kelley DS, Karson JA, Früh-Green GL et al (2005) A serpentinite-hosted ecosystem: the Lost City hydrothermal field. Science 307:1428-434 CrossRef
    49. Kelley DS, Karson JA, Donna K et al (2001) An off-axis hydrothermal field near the Mid-Atlantic Ridge at 30°N. Nature 412:145-49 CrossRef
    50. Ludwig KA, Kelley DS, Butterfield DA et al (2006) Formation and evolution of carbonate chimneys at the Lost City hydrothermal field. Geochim Cosmochim Acta 70:3625-645 CrossRef
    51. Früh-Green GL, Kelley DS, Bernasconi SM et al (2003) 30,000?years of hydrothermal activity at the Lost City vent field. Science 301:495-98 CrossRef
    52. Foustoukos DI, Savov IP, Janecky DR (2008) Chemical and isotopic constraints on water/rock interactions at the Lost City hydrothermal field, 30°N Mid-Atlantic Ridge. Geochim Cosmochim Acta 72:5457-474 CrossRef
    53. Fu Q, Lollar SL, Horita J et al (2007) Abiotic formation of hydrothermal under hydrothermal conditions: constraints from chemical and isotope data. Geochim Cosmochim Acta 71:1982-998 CrossRef
    54. Münch U, Lalou C, Halbach P et al (2001) Relict hydrothermal events along the super-slow Southwest Indian spreading ridge near 63°56′E—mineralogy, chemistry and chronology of sulfide samples. Chem Geol 177:341-49 CrossRef
    55. Tivey MA, Rona PA, Schouten H (1993) Reduced crustal magnetization beneath the active sulfide mound, TAG hydrothermal field, Mid-Atlantic Ridge at 26°N. Earth Planet Sci Lett 115:101-15 CrossRef
    56. Tivey MA, Schouten HK, Martin C (2003) A near-bottom magnetic survey of the Mid-Atlantic Ridge axis at 26°N: implications for the tectonic evolution of the TAG segment. J Geophys Res 108:2277 CrossRef
    57. Bach W, Banerjee NR, Dick HJB et al (2002) Discovery of ancient and active hydrothermal systems along the ultra-slow spreading Southwest Indian Ridge 10°E-6°E. Geochem Geophys Geosyst 3:1-0 CrossRef
    58. Banerjee R, Dick JBH, Wolfgang B et al (2001) Discovery of peridotitehosted hydrothermal deposits along the ultraslow-spreading Southwest Indian Ridge. In: Geological Society of America annual meeting, Boston, p 800
    59. Tuchkolke BE, Behn MD, Buck WR et al (2008) Role of melt supply in oceanic detachment faulting and formation of megamullions. Geology 36:455-58 CrossRef
    60. Blackman DK, Canales JP, Harding A (2009) Geophysical signatures of oceanic core complexes. Geophys J Int 178:593-13 CrossRef
  • 作者单位:Chunhui Tao (1)
    Huaiming Li (1)
    Xiaobing Jin (1)
    Jianping Zhou (1) (2)
    Tao Wu (1)
    Yonghua He (1)
    Xianming Deng (1)
    Chunhua Gu (1)
    Guoyin Zhang (1)
    Weiyong Liu (1)

    1. Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, State Oceanic Administration, Hangzhou, 310012, China
    2. Faculty of Resources, China University of Geosciences, Wuhan, 430074, China
  • ISSN:1861-9541
文摘
Polymetallic sulfides have attracted more attentions, which are regarded as one of the potential seabed mineral resources for their high grade of precious metal elements such as Cu, Zn, Pb, Au, and Ag. Since 2007, there are four China dayang cruises (CDCs) with eight legs totally, which have been carried out to investigate polymetallic sulfides on the southwest Indian ridge (SWIR), and eight hydrothermal vents have been found. In 2011, the China Ocean Mineral Resources Research and Development Association (COMRA) and International Seabed Authority (ISA) signed a 15-year contract for exploration for polymetallic sulfides located on the SWIR between 46°S and 53°S. The area allocated to the COMRA is approximately 10,000?km2. In this paper, we review the recent research advances about hydrothermal activity of the SWIR by the CDCs. As for the sulfides exploration in the future, some aspects should be emphasized, such as the controlling factors of sulfide mineralization on the SWIR, prospecting methods of inactive and buried sulfide deposits, sulfides resources assessment method, and the near-bottom sulfides exploration technology systems.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700