IODP中的海陆对比和海陆相互作用
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摘要
综合大洋钻探计划(IODP)将于2003年10月启动。与大洋钻探计划(ODP)相比,IODP规模更大,钻探和研究范围更宽,囊括地球科学的诸多领域,涉及海底生物圈、地球壳幔结构、俯冲工厂和地震活动、古环境记录和海底资源等。从海陆对比和海陆相互作用的角度,分析我国地球科学,尤其是新生代地质学研究中的一些特点和优势。中国新生代地质演化历史别具特色,如宏观地形格局的变化,喜马拉雅山和青藏高原的隆升,西太平洋边缘海的扩张,亚洲季风系统的形成等,这些特色成为中国科学家参与IODP科学研究计划的优势。
Integrate Ocean Drill Program (IODP) will be initiated in the year 2003. Compared with ODP, the scientific scope of IODP is much wider, covering more extensive sea floor and research disciplines, including deep ocean biosphere, mental and crust structure, subduction factory and seismology, global changes, and ocean resources. This paper will review some advantageous aspects of geoscience research in China, focusing on Cenozoic geological history such as the evolution of the overall topography of China, the uplift of Himalaya and Tibetan Plateau, the opening of the west Pacific marginal seas, and the establishment of the Asian monsoon system. The characteristics of the Cenozoic geology in China form the base for Chinese geologists to be involved in international collaboration during the course of IODP.
Integrate Ocean Drill Program (IODP) will be initiated in the year 2003. Compared with ODP, the scientific scope of IODP is much wider, covering more extensive sea floor and research disciplines, including deep ocean biosphere, mental and crust structure, subduction factory and seismology, global changes, and ocean resources. This paper will review some advantageous aspects of geoscience research in China, focusing on Cenozoic geological history such as the evolution of the overall topography of China, the uplift of Himalaya and Tibetan Plateau, the opening of the west Pacific marginal seas, and the establishment of the Asian monsoon system. The characteristics of the Cenozoic geology in China form the base for Chinese geologists to be involved in international collaboration during the course of IODP.
引文
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[4] WangPinxian.Fiftymillionsyears—Theoriginofthemodernenvironmentalsystem[J].Science,1997,49(3):18 22.[汪品先.上下五千万年———现代自然环境宏观格局的由来[J].科学,1997,49(3):18 22.]
[5] WangPinxian.Asiantopographicchange—Relationshipbetweenclimatesandtectonics[J].QuaternaryScience,1998,3:213221.[汪品先.亚洲形变与全球变冷———探索气候与构造的关系[J].第四纪研究,1998,3:213 221.]
[6] RuddimanWF,KutzbachJE.ForcingoflateCenozoicnorthernhemisphereclimatebyplateauupliftinsouthernAsiaandtheAmericanwest[J].JournalofGeophysicalResearch,1989,94(D15):18409 18427.
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[8] ZhuXia.TectonicsandEvolutionofMesozoicandCenozoicBasinsinChina[M].Beijing:SciencePress,1983.1 230.[朱夏.中国中新生代盆地构造和演化[M].北京:科学出版社,1983.1 230.]
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[10] PowellCM.ContinentalunderplatingmodelfortheriseoftheTibetanPlateau[J].EarthandPlanetaryScienceLetters,1986,81:79 94.
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[12] ChangC,etal.TheRoyalSociety/AcademiaSinica1985geotraverseofTibet Preliminaryconclusions[J].Nature,1986,323:501 504.
[13] ZhaoW,MorganWJ.UpliftofTibetPlateau[J].Tectonics,1985,4:359 371.
[14] EnglandP,MolnarP.Surface,upliftofrocks,andexhumationofrocks[J].Geology,1990,18:1173 1177.
[15] KutzbachJE,GuetterPJ,RuddimanWF,etal.ThesensitivityofclimatetolateCenozoicupliftinsouthernAsiaandtheAmericanwest:Numericalexperiments[J].JoumalofGeophysicalResearch,1989,94(D15):18393 18407.
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[17] PrellWL,KutzbachJE.SensitivityoftheIndianmonsoontoforcingparametersandimplicationsforitsevolution[J].Nature,1992,360:647 652.
[18] HarrisonTM,CopelandP,KiddWSF,etal.RaisingTibet[J].Science,1992,255:1663 1670.
[19] BurbankDW,DerryLA,France LanordC.ReducedHimalayansedimentproduction8Maagodespiteanintensifiedmonsoon[J].Nature,1993,364:48 50.
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[22] JiHongxiang,HuangWanbo,ChenWanyong,etal.ThediscoveryoftheHipparionfaunasinXizanganditssignificanceontheproblemoftheupliftofthePlateau[A].In:AcademiaSinicaTibetExpeditionTeam,eds.Age,Magnitude,andFormsoftheUpliftofTibetanPlateau[C].Beijing:SciencePress,1981.19 25.[计宏祥,黄万波,陈万勇,等.西藏三趾马动物群的首次发现及其对高原隆起的意义[A].见:中国科学院青藏高原综合科学考察队 青藏高原隆起的时代、幅度和形式问题[C].北京:科学出版社,1981.19 25.]
[23] XuRen OnpalaeobotanicalevidenceforcontinentaldriftandtheHimalayanuplift[A].In:AcademiaSinicaTibetExpeditionTeam,eds.Age,Magnitude,andFormsoftheUpliftofTibetanPlateau[C].Beijing:SciencePress,1981.8 18.[徐仁.大陆漂移与喜马拉雅山上升的古植物学证据[A].见:中国科学院青藏高原综合科学考察队.青藏高原隆起的时代、幅度和形式问题[C].北京:科学出版社,1981.8 18.]
[24] LiJ.TheUpliftoftheQinghai XizangPlateauanditsEffectonEnvironment[M].Beijing:SciencePress,1991.265 272.
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[26] FangXiaomin,LiJijun,ZhuJunjie.MagnetostratigraphyandtectoniceventsoftheWanjiashasection,Linxia[A].In:Formation,EnvironmentalEvolutionandEcologicalStudyofTibetanPlateau[C].Beijing:SciencePress,1995.65 73.[方小敏,李吉均,朱俊
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