地球科学进展 ›› 2003, Vol. 18 ›› Issue (5): 722 -729. doi: 10.11867/j.issn.1001-8166.2003.05.0722

研究论文 上一篇    下一篇

IODP中的海陆对比和海陆相互作用
郑洪波 1,2   
  1. 1.同济大学海洋与地球科学学院,上海 200092;2.中国科学院地球环境研究所,陕西 西安 710054
  • 收稿日期:2003-06-23 修回日期:2003-07-04 出版日期:2003-12-20
  • 通讯作者: 郑洪波 E-mail:zhenghb@mail.tongji.edu.cn
  • 基金资助:

    国家自然科学杰出青年基金项目“中国内陆干旱化的阶段性发展及机制”(编号:40025107);国家自然科学基金重点项目“西昆仑山前盆地演化反映的高原隆升与环境变迁”(编号:90211019);国家重点基础研究发展规划项目“地球圈层相互作用中的深海过程和深海记录”(编号:G2000078500);教育部“长江特聘教授/计划”项目资助.

LAND-OCEAN COMPARISON AND INTERACTIONS IN IODP

Zheng Hongbo 1,2   

  1. 1. School of Ocean and Earth Science, Tongji University, Shanghai 200092,China;2. Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710054,China
  • Received:2003-06-23 Revised:2003-07-04 Online:2003-12-20 Published:2003-10-01

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.

中图分类号: 

[1] Jin Xingchun, Zhou Zuyi, Wang Pinxian. Ocean Drilling Program and China Geoscience [M]. Shanghai: TongJi University Press, 1995. 1-349.[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,1995.1-349 .]

[2] Wang P X, Prell W L, Blume P. Proceedings of ODP Initial Reports 184 [M]. College Station TX (Ocean Drilling Program), 1999. 1-77.

[3] Earth, Ocean and Life-Integrated Ocean Drilling Program, Initial Science Plan, 2 003-2 013.

[4] Wang Pinxian. Fifty millions years—The origin of the modern environmental system [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] Wang Pinxian. Asian topographic change—Relationship between climates and tectonics [J]. Quaternary Science, 1998, 3: 213-221. [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] Ruddiman W F, Kutzbach J E. Forcing of late Cenozoic northern hemisphere climate by plateau uplift in southern Asia and the American west[J]. Journal of Geophysical Research, 1989,94(D15): 18 409-18 427.

[7] Ruddiman W F, ed. Tectonic Uplift and Climatic Change[M]. New York: Plenum Press, 1997. 1-535.

[8] Zhu Xia. Tectonics and Evolution of Mesozoic and Cenozoic Basins in China [M]. Beijing: Science Press, 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.]

[9] Powell C M, Conaghan P J. Plate tectonics and the Himalayas[J]. Earth and Planetary Science Letters, 1973, 20: 1-12.

[10] Powell C M. Continental underplating model for the rise of the Tibetan Plateau[J]. Earth and Planetary Science Letters, 1986, 81: 79-94.

[11] Tapponnier P, Molnar P. Slip-line field theory and large-scale continental tectonics[J]. Nature, 1976, 264: 319-323.

[12] Chang C, et al. The Royal Society/Academia Sinica 1985 geotraverse of Tibet-Preliminary conclusions[J]. Nature, 1986, 323: 501-504.

[13] Zhao W, Morgan W J. Uplift of Tibet Plateau[J]. Tectonics, 1985, 4: 359-371.

[14] England P, Molnar P. Surface, uplift of rocks, and exhumation of rocks[J]. Geology, 1990, 18: 1 173-1 177.

[15] Kutzbach J E, Guetter P J, Ruddiman W F, et al. The sensitivity of climate to late Cenozoic uplift in southern Asia and the American west: Numerical experiments[J]. Joumal of Geophysical Research, 1989, 94 (D15): 18 393-18 407.

[16] Raymo M E, Ruddiman W F. Tectonic forcing of late Cenozoic climate[J]. Nature, 1992, 359: 117-122.

[17] Prell W L, Kutzbach J E. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution[J]. Nature, 1992, 360: 647-652.

[18] Harrison T M, Copeland P, Kidd W S F, et al. Raising Tibet[J]. Science, 1992, 255: 1 663-1 670.

[19] Burbank D W, Derry L A, France-Lanord C. Reduced Himalayan sediment production 8 Ma ago despite an intensified monsoon[J]. Nature, 1993, 364: 48-50.

[20] Copeland P, Harrison T M. Episodic rapid uplift in the Himalayas revealed by 40Ar/39Ar analysis of detrital K-feldspar and muscovite, Bengal fan[J]. Geology, 1990, 18: 354-357.

[21] Molnar P, Burchfiel B C, Lian K, et al. The geologic evolution of northern Tibet: Results of an expedition to Ulugh Muztagh[J]. Science, 1987, 235: 299-305.

[22] Ji Hongxiang, Huang Wanbo, Chen Wanyong, et al. The discovery of the Hipparion faunas in Xizang and its significance on the problem of the uplift of the Plateau[A]. In: Academia Sinica Tibet Expedition Team, eds. Age, Magnitude, and Forms of the Uplift of Tibetan Plateau[C]. Beijing: Science Press, 1981. 19-25. [计宏祥,黄万波,陈万勇,. 西藏三趾马动物群的首次发现及其对高原隆起的意义[A]. :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] Xu Ren. On palaeobotanical evidence for continental drift and the Himalayan uplift[A]. In: Academia Sinica Tibet Expedition Team, eds. Age, Magnitude, and Forms of the Uplift of Tibetan Plateau[C]. Beijing: Science Press, 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]. : 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] Li J. The Uplift of the Qinghai-Xizang Plateau and its Effect on Environment[M]. Beijing: Science Press, 1991. 265-272.

[25] An Z S, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since late Miocene times[J]. Nature, 2001, 411: 62-66.

[26] Fang Xiaomin, Li JiJun, Zhu JunJie. Magnetostratigraphy and tectonic events of the WanJiasha section, Linxia[A]. In: Formation, Environmental Evolution and Ecological Study of Tibetan Plateau[C]. Beijing: Science Press, 1995. 65-73.[方小敏,李吉均,朱俊杰. 临夏盆地中心王家山剖面磁性地层与构造事件[A]. :青藏项目专家委员会编. 青藏高原形成演化、环境变迁与生态系统研究[C]. 北京:科学出版社,1995. 65-73.]

[27] Zheng H, Powell C, An Z, et al. Pliocene uplift of the northern Tibetan Plateau [J]. Geology, 2000, 28(8): 715-718.

[28] Tapponnier P, Molnar P. Active faulting and tectonics in China[J]. Journal of Geophysical Research, 1977, 82: 2 905-2 930.

[29] Tapponnier P, Peltzer G, Le Dain A, et al. Propagating extrusion tectonics in Asia: New insight from simple experiments with plasticine[J]. Geology, 1982, 10: 611-616.

[30] Pelzer G, Tapponnier P. Formation and evolution of strike-slip faults, rifts and basins during the India-Asia collision: An experimental approach[J]. Journal of Geophysical Research, 1988, 93: 15 095-15 117.

[31] Taylor B, Hayes D E. The tectonic evolution of the South China Sea basin[J]. AGU Geophysical Monograph, 1980, 23: 89-125.

[32] Taylor B, Hayes D E. Origin and history of the South China Sea basin[J]. AGU Geophysical Monograph, 1983, 27: 23-56.

[33] Holloway N H. North Palawan Block, Philippines - Its relation to Asian mainland and role in evolution of South China Sea[J]. American Association of Petroleum Geologists Bulletin, 1982, 66: 1 355-1 383.

[34] Karig D E. Origin and development of marginal basins in the western Pacific[J]. Journal of Geophysical Research, 1971,76:2 542-2 561.

[35] Zhang Kang. Ages of the drainages in the middle reaches of the Yellow river [J]. Quaternary Science in China, 1989, 8(1): 185-193. [张抗. 黄河中游水系形成史初探 [J]. 第四纪研究,1989, 81: 185-193.]

[36] Yue Leping, Lei Xiangyi, Qu Hongjun. Ages of the middle reaches of the Yellow River [J]. Geological Review, 1997, 43(2): 186-192. [岳乐平,雷祥义,屈红军. 黄河中游水系的阶地发育时代 [J]. 地质论评,1997, 43(2): 186-192.]

[37] Wu Xihao, Jiang Fuchu, Wang Sumin, et al. On the running through of Yellow river through Sanmenxia [J]. Quaternary Science, 1998, 2: 188. [吴锡浩,蒋复初,王苏民,. 关于黄河贯通三门峡东流入海问题 [J]. 第四纪研究,1998,2: 188.]

[38] Milliman J D, Meade R H. World-wide delivery of river sediment to the oceans[J]. Journal of Geology, 1983, 91: 1-21.

[39] Zheng Hongbo, Kutherine Butcher, Chris Powell. Evolution of Neogene foreland Basin in Yecheng, XinJiang, and uplift of northern Tibetan Plateau I- stratigraphy and petrology [J]. Acta Sedimentologica Sinica, 2002, 20(2): 274-281. [郑洪波, Kutherine Butcher, Chris Powell. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升 —I 地层学与岩石学证据 [J].沉积学报, 2002, 20(2): 274-281.]

[40] Zheng Hongbo, Kutherine Butcher, Chris Powell. Evolution of Neogene foreland Basin in Yecheng, XinJiang, and uplift of northern Tibetan Plateau II- Facies analysis [J]. Acta Sedimentologica Sinica, 2003, 21(1): 46-51.[郑洪波, Kutherine Butcher, Chris Powell. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升—II 沉积相与沉积盆地演化[J].沉积学报,2003, 21(1): 46-51.]

[41] Clift P, Clark M K, Royden L H. An erosional record of Tibetan Plateau uplift and the Asian Monsoon in the East Asian marginal seas[J]. EOS, Transactions of Fall Meeting, AGU,Supple,2002,83(47).

[42] Clift P D, Gaedicke C. Accelerated mass flux to the Arabian Sea during the Middle-Late Miocene[J]. Geology, 2002, 30: 207-210.

[43] Pettke T, Halliday A N, Hall C M, et al. Dust production and deposition in Asia and the North Pacific Ocean over the past 12 Ma[J]. Earth and Planetary Science Letters, 2000, 178:1-17.

[44] Rea D K, Snoeckx H, Joseph L H. Late Ceonozoic eolian deposition in the North Pacific: Asia drying, Tibetan uplift and cooling of the Northern Hemisphere[J]. Paleoceanography, 1998, 13: 215-224.

[45] Liu Tungsheng, et al. Loess and the Environment [M]. Beijing: Science Press, 1985. 1-481. [刘东生,.黄土与环境 [M]. 北京:科学出版社, 1985. 1-481.]

[46] An Z S, Liu T S, Lu Y C, et al. The long term paleomonsoon variation recorded by the loess-paleosol sequence in central China[J]. Quaternary International, 1990,7/8: 91-95.

[47] Guo Z T, Ruddiman W, Hao Q Z, et al. Onset of Asian desertification by 22 Ma ago inferred from loess deposits in China[J]. Nature, 2002, 416: 159-163.

[48] Ding Z L, Yang S L, Sun J M, et al. Iron geochemistry of loess and red clay deposits in the Chinese Loess Plateau and implications for long-term Asian monsoon evolution in the last 7.0 Ma[J]. Earth and Planetary Science Letters, 2001, 185: 99-109.

[49] Wang L, Sarnthein M, Erlenkeuser H, et al. East Asian monsoon climate during the Late Pleistocene: High-resolution sediment records from the South China Sea[J]. Marine Geology, 1999, 156: 245-284.

[50] Jian Z, Zhao Q, Cheng X, et al. Pliocene-Pleistocene stable isotope and paleoceanographic changes in the northern South China Sea[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, 193(3/4): 425-442.

[51] Wang Pinxian, Tian Jun, Cheng Xinrong. Transition of Quaternary glacial cyclicity in deep-sea records at Nansha, the South China Sea [J]. Science in China (D), 2001, 44 (10): 926-933. [汪品先, 田军, 成鑫荣. 第四纪冰期旋回转型在南沙深海的记录[J]. 中国科学:D, 2001, 31(10): 793-799.]

[52] Zheng H B, Powell C, Rea D, et al. Late Miocene and mid-Pliocene enhancement of the East Asian Monsoon as viewed from land and sea[J]. Global and Planetary Change (in press).

[53] Yang Zigeng. Evolution of shelf of China in Quaternary and its environmental consequences[A]. In: Liang Mingsheng, Zhang Jilin, eds. Comparison of Marine and Continent in China[C]. Beijing: Science Press, 1991. 1-22. [杨子赓. 中国东部陆架第四纪时期的演变及其环境效应[A]. :梁名胜,张吉林主编.中国海陆第四纪对比研究[C]. 北京:科学出版社,1991. 1-22.]

[54] Wang P X. Response of Western Pacific marginal seas to glacial cycles: Paleoceanograpic and sedimentological features[J]. Marine Geology, 1999, 156: 5-39.

[55] Qin Yunshan, Zhao Songling. New progress in study of sedimentation model of China's shelf area[A]. In: Liang Mingsheng, Zhang Jilin, eds. Comparison of Marine and Continent in China[C]. Beijing: Science Press, 1991. 23-39. [秦蕴珊,赵松龄. 中国陆架沉积模式研究的新进展[A]. :梁名胜,张吉林主编.中国海陆第四纪对比研究[C]. 北京:科学出版社, 1991. 23-39.]

No related articles found!
阅读次数
全文


摘要