大洋钻探与深海热液作用

doi:10.11867/j.issn.1001-8166.1995.03.0223

地球科学进展 ›› 1995, Vol. 10 ›› Issue (3): 223 -228. doi: 10.11867/j.issn.1001-8166.1995.03.0223

大洋钻探与深海热液作用

吴世迎

国家海洋局第一海洋研究所青岛 266003

收稿日期:1995-02-21 出版日期:1995-06-01
通讯作者: 吴世迎

OCEAN DRILLING AND DEEP-SEA HYDROTHERMAL ACTIVITY

Wu Shiying

First Institute of Oceanography,SOA,Qingdao 266003

Received:1995-02-21 Online:1995-06-01 Published:1995-06-01

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在DSDP/ODP的26年钻探中，有近20个航次钻遇到热液作用踪迹或热液产物。强调了深海热液作用作为研究海底扩张、地幔物质上涌、新生洋壳生成及火山活动所构成的地壳演化过程，已经成了大洋钻探计划的核心内容之一，并由此在若干重大理论问题上，获得了突破性的发展。

关键词: 大洋钻探, 热液作用, 海水循环, 成矿源

Deep-sea hydrothermal activities and hydrothermal products which were found during nearly 20 cruises in the past 26 years of DSDP/ODP are introduced. It is emphasized that deep-sea hydrothermal activity, as the study of sea-floor spreading, mantle material upwelling, new ocean-floor formation and volcanic activities, has been one of the core aspects in the Ocean Drilling Project. With the study of deep-sea hydrothermal activity, a break through progress has been obtained in many important theoretical problems.

Key words: Ocean Drilling, Hydrothermal activity, Sea-water circulation, Mineralization sources.

[1] Rona P A. Polymetallic sulfides at seafloor spreading centers:A global overiew. Marine Technology Society Journal，1982,16:81-81.
[2] Bearman G. The ocean basins:Their structure and evolution. Open University Series, (Hrsg.).1988. 171pp.
[3] Honnorez J, Von Herzen R P et al. Hydrothermal mounds and young ocean crust of the Galapagos,Preliminary Deep Sea Drilling results,Leg 70. Geol Soc America Bull,1981,92:457-472.
[4] Gillis K,Mevel C & Allan J. Hess deep rift valley. Joides Journal,1993,19(2):17-22.
[5] Alt J C,Kinoshita H & Stocking L. Return to hole 504B.Joides Journal,1993,19(3):9-14.
[6] Pezard P. Return to hole 504B. Joides Journal,1993,19(3):15-16.
[7] Meyer P S & Gillis K M. Oceanic crust composition and structure. Oceanus,1993/94,36(4):70-74.
[8] Von Stacklberg U & Von Rad U. Geological evolution and hydrothermal activity in the Lau and North Fiji Basins (SONNE cruise SO-35)-a synthesis.Geol Jr, Hannover,1990,D92,629-660.
[9] Natland J H & Hekinian R. Hydrothermal alteration of basalts and sediments at Deep Sea Drilling Project Site 456,Mariana Trough. Initial Reports of the Deep Sea Drilling Project 60,1982.759-766.
[10] Craig H,Horibe Y & Farley K A. Hydrothermal vents in the Mariana Trough,results of the first Alvin dives. EOS, 1987,68:1531.
[11] 吴世迎主编.马里亚纳海槽海底热液烟囱和菲律宾海沉积物.北京:海洋出版社，1991.193pp.
[12] Karson J A,Cannat M & Miller D J. Drilling in the Western Wall of the Mark area. Joides Journal, 1993,19(3): 26-28.
[13] Rabinowitz P D, Francis T J G et al. Ocean Drilling Program: Results from eighth year of drilling operations. Offshore Teachnology Conference at the 25th Annual OTC in Houston,Texas. USA. 3-6 May 1993.OTC7082,59-81.
[14] Kastner M & Martin J B. Fluid composition in subduction zones. Oceanus, 1993/94,36(4):87-90.
[15] Pezard P A. DSDP/ODP downhole measurements in Hole 504B. Oceanus, 1993/94,36(4):79-81.
[16] Chamley H. Clay Sedimentology. Berlin: Springer, 1989. 623pp.
[17] Kypносов B Е.Гидротермалвные изменения базальтов коры океана.Тихоокеанская Геолояия,1984,(6):90-94.
[18] Lalou C, Thompson G,Rona P A, Brichet E & Jehanno C.Chronology of selected hydrothermal Mn oxide deposits from the trans-Atlantic geotraverse "TAG"area,Mid-Atlantic Ridge 26°N.Geoch Cosmoch Acta, 1986,50:1737-1743.
[19] 郭锋，张雨编译.美国国家海洋和大气局研究全球性海底热液变化的战略规划.海洋地质动态,1990,(5) :13-14.
[20] Цущаровский Ю М,Еазилевская Е С, Косшинская И П.Проблемы геологии Мировсгс океана.Содержание,1985,(5):36-44.
[21] Chen J C & Owen R M. The hydrothermal component in ferromanganese nodules from the southeast Pacific Ocean. Geoch Cosmoch Acta,1989,53:1299-1305.

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