DEEP-SEA HYDROTHERMAL ACTIVITY: A HOT RESEARCH TOPIC

XIA Jian-xin; LI Chang; MA Yan-fang

2007 Vol. 13, No. 2

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XIA Jian-xin, LI Chang, MA Yan-fang. DEEP-SEA HYDROTHERMAL ACTIVITY: A HOT RESEARCH TOPIC[J]. Journal of Geomechanics, 2007, 13(2): 179-191, 118.

Citation:

XIA Jian-xin, LI Chang, MA Yan-fang. DEEP-SEA HYDROTHERMAL ACTIVITY: A HOT RESEARCH TOPIC[J]. Journal of Geomechanics, 2007, 13(2): 179-191, 118.

DEEP-SEA HYDROTHERMAL ACTIVITY: A HOT RESEARCH TOPIC

College of Life and Environmental Science, Central University of Nationalities, Beijing 100081, China

Received Date: 25 January 2007

Publish Date: 25 June 2007

Abstract

Abstract

Deep seafloor hydrothermal activity is a hot frontier research topic of modern marine geoscience.In China research on this aspect just begins and it is very necessary to summarize the available research results.This paper reviews the history and current state of the study of seafloor hydrothermal activities, with the focus on the analysis of the results of theoretical research on the dynamic process of hydrothermal venting.The authors found various factors that affect the shapes and distribution of hydrothermal plumes from various field measurements of events and analyzed various hot topics of oceanographic research such as hydrothermal black smokers and extreme ophiles, which provides a basis for the investigation and theoretical study of deep-sea hydrothermal activity.
- seafloor hydrothermal fluids /
- hydrothermal plume /
- tidal currents /
- extreme ophiles /
- black smoker

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References

[1]	Rona PA, Scott SD.A special issue on sea floor hydrothermal mineralization:new perspectives [J].Economic Geology, 1993, 1935~1976. Google Scholar
[2]	Hannington MD, Herzig P, Stoff'ers P, et al.First observations of high-temperature submarine hydrothermal vents and massive anhydrite deposits off the north coast of Iceland [J].Marine Geology, 2001, 177 :199~220. doi: 10.1016/S0025-3227(01)00172-4 CrossRef Google Scholar
[3]	王兴涛. 现代海底热液活动的热液循环及烟囱体研究[D]. 青岛: 中国海洋大学, 2004, 10~20.http://www.wanfangdata.com.cn/details/detail.do?_type=degree&id=Y646737 Google Scholar
[4]	季敏, 瞿世奎.现代海底典型热液活动区地形环境特征分析[J].海洋学报, 2005, 27 (6):46~55. doi: 10.3321/j.issn:0253-4193.2005.06.007 CrossRef Google Scholar
[5]	栾锡武.现代海底热液活动区的分布与构造环境分析[J].地球科学进展, 2004, 19 (6):931~938 doi: 10.3321/j.issn:1001-8166.2004.06.010 CrossRef Google Scholar
[6]	Edmonds HN, Michael P J, Baker ET.Discovery of abundant hydrothermal venting on the ult raslow-spreading Gakkel ridge in the Arctic Ocean [J].Nature, 2003, 421:252~272. doi: 10.1038/nature01351 CrossRef Google Scholar
[7]	Butterfield DA, Massoth GJ.Geochemistry of North Cleft segment vent fluids:temporal changes in chlorinity and their possible relation to recent volcanism [J].Geophs Res, 1994, 99 :4951~4968. doi: 10.1029/93JB02798 CrossRef Google Scholar
[8]	Von Damm KL, Buttennore LG, Oosting SE.Direct observation of the evolution of a seafloor black smoker from vapor to brine [J]. EPSL, 1997, 149 :101~111. doi: 10.1016/S0012-821X(97)00059-9 CrossRef Google Scholar
[9]	杜同军, 翟世奎, 任建国, 等.海底热液活动与海洋科学研究[J].青岛海洋大学学报, 2002, 32 (4):597~602 doi: 10.3969/j.issn.1672-5174.2002.04.027 CrossRef Google Scholar
[10]	Jean-Baptiste P, BougaulT H.海底热液活动和海底热源[J].国外铀金地质, 1992, 4 :36~38. Google Scholar
[11]	栾锡武, 赵一阳, 秦蕴珊, 等.热液系统输向大洋的热通量估算[J].海洋学报, 2002, 24 (6):60~67. Google Scholar
[12]	栾锡武, 翟世奎, 干晓群, 等.冲绳海槽中部热液活动区构造地球物理特征分析[J].沉积学报, 2001, 19 (1): 43~47. doi: 10.3969/j.issn.1000-0550.2001.01.007 CrossRef Google Scholar
[13]	李江海, 牛向龙, 冯军.海底黑烟囱的识别研究及其科学意义[J].地球科学进展, 2004, 19 (1):17~25. doi: 10.3321/j.issn:1001-8166.2004.01.003 CrossRef Google Scholar
[14]	栾锡武, 赵一阳, 秦蕴珊.热液柱的形态研究[J].热带海洋学报, 2002, 21 (2):91~97. doi: 10.3969/j.issn.1009-5470.2002.02.011 CrossRef Google Scholar
[15]	Elderfield H, Wheat CG, Mottl MJ, et al.Fluid and geochemical transport through oceanic crust:A transect across the eastern flank of the Juan de Fuca Ridge [J].Earth and Planetary Science Letters, 1999, 172 (1~2):151~165. doi: 10.1016/S0012-821X(99)00191-0 CrossRef Google Scholar
[16]	Goodman JC, Collins GC.Hydrothermal Plume Dynamics on Europa:Implications for Chaos Formation [J].Journal of Geophisical Research, 2002, 1:1~47. Google Scholar
[17]	Wichers S. Verifi cation of Numerical Models for Hydrothermal Plume Water Through Field Measurements at TAG. http://econscience.org/scott/pubs/thesis.pdf (Viewed Oct 2006). Google Scholar
[18]	Prui sMH, Hautala SL, Johnson HP et al. Turbulent heat flux in the deepocean above diffuse hydrothermal vents. http://www.nwra.com/resumes/pruis/Pruisetal_deepsea_2004.pdf (Viewed Oct 2006). Google Scholar
[19]	Butterfield DA., Seyfried WE Jr.and Lilley MD.Composition and evolution of hydrothermal fluids [J].Energy and Mass Transfer in Marine Hydrothermal Systems.2003, 123~162. Google Scholar
[20]	Speer KG, Marshall J.The growth of convective plumes at sea floor hot springs [J].J.Marine Res., 1995, 53 :1025~1057. doi: 10.1357/0022240953212972 CrossRef Google Scholar
[21]	Gill AE. Atmosphere-Ocean Dynamics [M]. Academic Press, 1982. Google Scholar
[22]	Pedlosky J. Geophysical Fluid Dynami cs [M]. Springer-Verlag, 1987. Google Scholar
[23]	王连捷, 张利容, 王薇, 等.地球自转速率变化引起的全球应力场[J].地质力学学报, 1997, 3 (3):12~20. Google Scholar
[24]	戴问天.海底热液作用的发现及其对地球科学的影响[J].西安地质学报, 1985, 7 (3):43~46. Google Scholar
[25]	常国显.地球化学中的一个新课题-洋脊热液循环作用[J].海洋通报, 1983, 2 (2):104~112. Google Scholar
[26]	Tivey MK.Hydrothermal vent systems [J].Oceanus, 1992, 34 :68~74. Google Scholar
[27]	Speer KG, Helfrich KR. Hydrothermal plumes: a review of flow and fluxes [A]. In: Parson LM, Walker CL, Dixon DR(eds), Hydrothermal Vents and Processes (87)[C]. London: Geological Society Special Publication, 1995, 373~385. Google Scholar
[28]	Pappalardo R et al.Does Europa have a subsurface ocean evaluation of the geologic evidence [J].Geophys.Res-Planets, 1999, 104:24015~24056. doi: 10.1029/1998JE000628 CrossRef Google Scholar
[29]	Turner JS.Turbulent entrainment :the development of the entrainment assumption and its appli cation to geophysi cal flows [J]. Fluid Mech, 1986, 173:431~471. doi: 10.1017/S0022112086001222 CrossRef Google Scholar
[30]	Marshall FS.Open ocean convection:observations, models and theory [J].Rev Geophysics, 1999, 37 :1~64. doi: 10.1029/98RG02739 CrossRef Google Scholar
[31]	Fernando HJS, Chen R, et al.Development of a point plume in the presence of background rotation [J].Phys Fluids, 1998, 10: 2369~2383. doi: 10.1063/1.869754 CrossRef Google Scholar
[32]	栾锡武, 秦蕴珊.现代海底热液活动的调查研究方法[J].地球物理学进展, 2002, 17 (4):592~597. doi: 10.3969/j.issn.1004-2903.2002.04.005 CrossRef Google Scholar
[33]	吴珍汉.略论引潮力的交变应力效应及其地球动力学意义[J].地质力学学报, 1998, 4 (3):20~27. Google Scholar
[34]	Pickard G., Emery WJ.Descriptive Physical Oceanography [M].New York:Pergamon Press, 1964, 662. Google Scholar
[35]	John E. Lupton, et al. 用RAFOS中性浮力漂流物追踪事件热液柱的演化[J]. Science, 1998, Vol. 280, No. 5366.http://lib.cqvip.com/qk/81668X/200001/3485643.html Google Scholar
[36]	Scheier DS, Baker ET, Johnson KT.Detection of hydrothermal plumes along the Southeast Indian Ridge near the Amsterdam St [J].Plateau Geophy Res Lett.1998, 25:97~100. doi: 10.1029/97GL03443 CrossRef Google Scholar
[37]	German CR, Baker ET, Mevel C.Hydrothermal activity along the southwest Indian ridge [J].Nature, 1998, 395:490~493. doi: 10.1038/26730 CrossRef Google Scholar
[38]	席峰, 郑天凌, 焦念志, 等.深海微生物多样性形成机制浅析[J].地球科学进展, 2004, 19 (2):38~44. Google Scholar
[39]	赵昌会, 叶德赞, 魏文玲.深海微生物的研究进展[J].微生物学通报, 2006, 33 (3):142~146. doi: 10.3969/j.issn.0253-2654.2006.03.028 CrossRef Google Scholar
[40]	钱江初, 于刚, 刘春秋, 等.Lost City低温热液场———一种新的海底热液活动类型[J].海洋学研究, 2006, 24 (1):43~49. doi: 10.3969/j.issn.1001-909X.2006.01.006 CrossRef Google Scholar
[41]	冯军, 李江海, 陈征."海底黑烟囱"与生命起源述评[J].北京大学学报(自然科学版), 2004, 40 (2):318~325. doi: 10.3321/j.issn:0479-8023.2004.02.020 CrossRef Google Scholar
[42]	Rise Project Group.East Pacific Rise:Hot springs and geophysical experiments [J].Science, 1980, 207:1421~1433. doi: 10.1126/science.207.4438.1421 CrossRef Google Scholar