科学大洋钻探：成就与展望

doi:10.11867/j.issn.1001-8166.2003.05.0666

在回顾ODP学术目标的发展历史的基础上，按照地球环境动力学和地球内部动力学两大科学主题，对ODP在地球环境变化、作为环境变化营力的沉积物、流体和细菌、地球内部物质和能量的传递、岩石圈变形和地震作用等前沿领域所取得的主要科学成就进行了简单的介绍。IODP将以地球系统科学的思想为指导，利用多个钻探平台，以更为广泛的钻探领域和更深的钻探深度，对全球海底进行学术目标更为庞大、系统的科学钻探，并进一步加强与石油工业以及其它国际地学研究计划的合作。

关键词: ODP, IODP, 科学成就, 科学目标

After a brief review of the evolution of scientific themes of ODP, major scientific achievements made by ODP are listed into two categories,i.e., dynamics of Earth’s environment and dynamics of Earth’s interior. Achievements made in fields such as Earth’s environment change, sediments, fluids and bacteria as the agents for environment change, mass and energy transfer of the Earth’s interior, lithosphere deformation and earthquake have changed our understanding of our dynamic Earth. IODP will follow the idea of Earth system science by proposing broader scientific themes and initiatives in a systematic way. Multiple platforms will enable IODP to drill deeper and in areas that were not accessible in ODP. Co-operations with industry and other international research programs in Earth science will be enhanced in the IODP phase.

Key words: Scientific achievements, Scientific themes., ODP, IODP

中图分类号:

[1] COSOD II. Report of the Second Conference on Scientific Ocean Drilling [R]. Strasbourg: Joint Oceanographic Institutions, Inc, 1987. 1-142.

[2] JOIDES Planning Committee. Understanding Our Dynamic Earth through Ocean Drilling[C]. JOI Inc, 1996.1-86.

[3] JOI.ODP Highlights[C]. Washington DC: JOI,2002.

[4] Shackleton N J, Crowhurst S, Hagelberg T, et al. A new late Neogene time scale: Application to Leg 138 sites[A]. In: Pisias N G, Mayer L A, Janecek T R, et al. Proceedings of ODP, Scientific Results, 138: College Station[C]. TX (Ocean Drilling Program), 1995.73-101.

[5] Raymo M. New insights into Earth’s history : An introduction to Leg 162 postcruise research published in Journals[A]. In: Raymo M, Jansen E, Blum P, et al, eds. Proceedings of the Ocean Drilling Program, Scientific Results[C]. 1999, 162: 273-275.

[6] IWG. Earth,Oceans and Life:Scientific Investigation of the Earth System Using Multiple Drilling Plateforms and New Technologies: IODP Initial Plan[R].Washington: International Working Group Support Office,2001.42-49.

[7] Verosub K L, Harris A H, Karlin R. Ultrahigh-resolution paleomagnetic record from ODP Leg 169S, Saanich Inlet, British Columbia: Initial results[J]. Marine Geology,2001,174(1/4):79-93.

[8] Zachos J C, Lohmann K C, Walker J C G, et al. Abrupt climate change and transient climates during the Paleogene: A marine perspective[J]. Journal of Geology, 1993, 101: 191-213.

[9] Deconto R M, Pollard D. Rapid Cenozoic glaciation of Antarctica induced by declining atmospheric CO₂[J]. Nature, 2003,421: 245-249.

[10] Pinxian Wang, Jun Tian, Xinrong Cheng, et al. Carbon reservoir changes preceded maJor ice-sheet expansion at the mid-Brunhes event[J]. Geology,2003,31(3): 239-242.

[11] ODP Leg 171B Shipboard Scientific Party. Critical boundaries in Earth's history-and the K-T boundary[J]. JOIDES Journal,1997,23(1):1-3.

[12] Miller K G. The role of ODP in understanding the causes and effects of global sea level change [J]. JOIDES Journal, 2002, 28 (1): 23-28.

[13] Cochran J R. Himalayan uplift, sea level, and the record of Bengal Fan sedimentation at the ODP Leg 116 sites[A]. In: Cochran J R, Stow D A V, et al, eds. Scientific Results Ocean Drilling Program[C]. 1990, 116: 397-414.

[14] D’Hondt S, Smith D C, Spivack A J. Exploration of the marine subsurface biosphere [J]. JOIDES Journal, 2002, 28 (1): 51-54.

[15] Pearce J. The oceanic lithosphere[J]. JOIDES Journal, 2002, 28 (1): 61-66.

[16] Jin Xingchun,Zhou Zuyi,Wang Pinxian. Ocean Drilling & Chinese Earth Science[M]. Shanghai:TongJi University Press,1995.223-265. [金性春,周祖翼,汪品先.大洋钻探与中国地球科学[M].上海:同济大学出版社,1995. 223-265.]

[17] von Huene R, Scholl D W. The return of Sialic material to the mantle indicated by terrigenous material subducted at convergent margins [J]. Tectonophysics, 1993 , 219: 163-175.

[18] Taylor B, Huchon P, Klaus A, et al. Active Continental Extension in The Western Woodlark Basin, Papua New Guinea, Ocean Drilling Program, Preliminary Reports, 180[R].1998.

[1]	赵玉龙, 刘志飞. 等积体在全球大洋中的空间分布及其古环境意义——国际大洋钻探计划对全球等深流沉积研究的贡献[J]. 地球科学进展, 2017, 32(12): 1287-1296.
[2]	张虎才. 参加国际大洋发现计划IODP 361的启示[J]. 地球科学进展, 2016, 31(4): 422-427.
[3]	李永祥，鄢全树，赵西西，全体船上科学家. 剥蚀型汇聚板块边缘大地震成因机理研究：来自国际综合大洋钻探344航次的报告[J]. 地球科学进展, 2013, 28(6): 728-736.
[4]	胡正莹，王汝建，李文宝. 南塔斯曼海隆2 Ma以来碳酸钙沉积记录及其对环流系统和轨道周期的响应[J]. 地球科学进展, 2013, 28(2): 269-281.
[5]	汪鹏，钟广法. 南海ODP1144站深海沉积牵引体的岩石物理模型研究[J]. 地球科学进展, 2012, 27(3): 359-366.
[6]	杨守业，王权. 冲绳海槽中部热液活动与IODP 331航次初步成果[J]. 地球科学进展, 2011, 26(12): 1282-1289.
[7]	朱俊江. 哥斯达黎加地震起源计划——IODP 334航次介绍[J]. 地球科学进展, 2011, 26(12): 1300-1305.
[8]	吴婷婷,李三忠,庞洁红,王健,戴黎明，IODP Expedition 324 Scientific Party. IODP 324航次FMS成像测井资料处理及其在Shatsky海隆构造研究中的应用[J]. 地球科学进展, 2010, 25(7): 753-765.
[9]	李春峰,苏新,姜涛,Ujiie K, Fabbri O, Yamaguchi A,Chester F M,Kimura G. 日本南海海槽俯冲增生楔前缘的构造变形特征[J]. 地球科学进展, 2010, 25(2): 203-211.
[10]	陈木宏. 国际综合大洋钻探计划IODP323白令海航次介绍[J]. 地球科学进展, 2009, 24(12): 1352-1356.
[11]	田军. 新生代的气候节律：赤道太平洋IODP-320、321航次[J]. 地球科学进展, 2009, 24(12): 1357-1361.
[12]	刘志飞，拓守廷. IODP计划的新进展[J]. 地球科学进展, 2009, 24(12): 1318-1324.
[13]	郑洪波,汪品先,刘志飞,杨守业,王家林,李前裕,周祖翼,贾军涛,李上卿,贾健宜,JohnChappell,YoshikiSaito,TakahiroInoue. 东亚东倾地形格局的形成与季风系统演化历史寻踪——综合大洋钻探计划683号航次建议书简介[J]. 地球科学进展, 2008, 23(11): 1150-1160.
[14]	李清,王家生,王晓芹,陈祈,陈洪仁. IODP 311航次底栖有孔虫碳稳定同位素对天然气水合物地质系统的指示[J]. 地球科学进展, 2008, 23(11): 1161-1166.
[15]	钟广法,李前裕,郝沪军,王嘹亮. 深水沉积物波及其在南海研究之现状[J]. 地球科学进展, 2007, 22(9): 907-913.

阅读次数

全文

摘要

SCIENTIFIC OCEAN DRILLING：ACHIEVEMENTS AND PROSPECTS