地球科学进展 ›› 2000, Vol. 15 ›› Issue (3): 297 -302. doi: 10.11867/j.issn.1001-8166.2000.03.0297

综述与评述 上一篇    下一篇

中国陆架 210Pb测年应用现状与思考
范德江,杨作升,郭志刚   
  1. 青岛海洋大学,山东 青岛 266003
  • 收稿日期:1999-06-07 修回日期:1999-08-13 出版日期:2000-06-01
  • 通讯作者: 范德江,男, 1965年3月出生于福建省闽清县,副教授,主要从事海洋沉积学研究。
  • 基金资助:

    国家自然科学基金项目“东海陆架远端软泥区物质汇作用”(编号: 49676289)资助。

REVIEW OF 210Pb DATING IN THE CONTINENTAL SHELF OF CHINA

FAN Dejiang,YANG Zuosheng,GUO Zhigang   

  1. Ocean University of Qingdao,Qingdao 266003,China
  • Received:1999-06-07 Revised:1999-08-13 Online:2000-06-01 Published:2000-06-01

分析总结了中国陆架210Pb测年现状及取得的成果,评价了210Pb测定沉积速率的可靠性。由于数据处理及成果表达的不统一,得到的沉积速率只能定性—半定量地表征沉积作用强度。根据210Pb测年现状、陆架沉积环境特征探讨了改善210Pb应用的有关问题,认为合理的选区、必要的校正、统一的成果表达是提高210Pb应用水平的重要因素。

The achievements and current situation of 210Pb dating in the continental shelf of China were summarized. The reliability of 210Pb dating for the sedimentary rate was commented. It is shown that the sedimentary rate calculated from 210Pb dating only qualitatively or semi-quantitatively responds to the real sedimentation strength, due to the ununity of data process and result expression. Based on the current situation of 210Pb dating, the characters of the sedimentary environment in the shelf, the problems how to improve the reliability of 210Pb dating for sedimentary rate are discussed and analyzed, indicating that the reasonabale selection of study area, necessary adjustment and unity of result expression are the important factors to improve the application of 210Pb dating in the continental shelf of China.

中图分类号: 

〔1〕Grozaz G, Picciotto E. Antarctic snow chronology with 210Pb〔J〕. Journal of Geophysical Research, 1964, 69(12): 2 597~2 604.
〔2〕Krishnaswami S, Lal D, Martin J M,et al. Geochronology of lake sediments〔J〕. Earth and Planetary Science Letters,1971,11:407~414.
〔3〕Robins J A, Edginton D N. Determination of resent sedimentation rates in Lake Michgan using 210Pb and137Cs〔J〕. Geochimica et Cosmochimica Acta, 1975, 39:285~304.
〔4〕Matsumoto S.210Pb geochronology of sediments from Lake Shiniji〔J〕. Geochimica Journal, 1975, 9: 167~172.
〔5〕Koide M, Soutar A, Goldberg E D,et al. Marine geochronology with 210Pb〔J〕. Earth Planetary Science Letters, 1972, 14: 442~446.
〔6〕Nittreouer C A, Sternberg R W, Carpenter R,et al. The use of 210Pb geochronology as a sedimentological tool: application to the Washinton continental shelf〔J〕. Marine Geology,1979, 31: 296~316.
〔7〕DeMaster D J, Mckee B A, Nittrouer C A,et al. Rates of sediment accumulation and particle reworking based on radiochemical measurements from continental shelf deposits in the East China Sea〔J〕. Continental Shelf Research, 1985, 4:143~158.
〔8〕邹汉阳,苏贤泽,余兴光,等.210Pb法测定东海大陆架现代沉积速率〔J〕.台湾海峡, 1982, 1(2): 30~40.
〔9〕曾文义,程汉良,姚建华,等。海洋沉积物中210Po的测定及其在地质年代学上的应用〔J〕.台湾海峡, 1983, 2(2): 30~36.
〔10〕业渝光,薛春汀,刁少波.现代黄河三角洲叶瓣模式的210Pb证据〔J〕.海洋地质与第四纪地质, 1987, 7(增刊): 75~80.
〔11〕李凤业.用210Pb测定南海陆架浅海沉积速率〔J〕.海洋科学,1988, 12(3): 64~66.
〔12〕李凤业,袁巍.渤海辽东湾现代沉积速率和沉积通量〔J〕.海洋科学集刊, 1990, 31: 267~273.
〔13〕李凤业,袁巍.南海、南黄海、渤海210Pb垂直分布模式〔J〕.海洋地质与第四纪地质,1991, 11(3): 35~43.
〔14〕Li Fengye, He Lijuan, Shi Yulan. Isotopic records of modern sedimentary environments in the Southern Yellow Sea〔A〕.Proceedings of the Korea-China International Seminar on Holocene and Pleistocene Environments in Yellow Sea Basin〔C〕.Seoul, Korea, 1996.151~157.
〔15〕邹汉阳,曾文义,程汉良,等.沉积物中210Pb、210Po和226Ra的分析及现代沉积速率的测定〔J〕.科学通报, 1985, 4(6):10~14.
〔16〕夏明,张承惠,马志邦,等.210Pb年代方法和珠江口、渤海锦州湾沉积速率的测定〔J〕.科学通报, 1983, 2(5): 291~295.
〔17〕苏贤泽,马文通,徐胜利,等.海洋沉积物的210Pb地质年代学方法〔J〕.台湾海峡, 1984, 3(1): 50~58.
〔18〕康兴伦.210Pb测年法的数据处理问题〔J〕.海洋科学, 1986,10(6): 13~17.
〔19〕钱江初.210Pb沉积速率的误差及校正〔J〕.东海海洋, 1987,5(3): 29~34.
〔20〕业渝光,和杰,刁少波,等.现代黄河三角洲210Pb剖面标准化方法——粒度相关法〔J〕.地理科学, 1992, 12(4): 279~286.
〔21〕Youn Jeung-Su. Clay mineralogy and radioactive isotope geochronology of continental shelf sediments around the Cheju Island, Korea〔A〕. Proceedings of the Korea-China International Seminar on Holocene and Pleistocene Environments in Yellow Sea Basin〔C〕. Seoul, Korea, 1996.151~157.
〔22〕金翔龙.东海海洋地质〔M〕.北京:海洋出版社, 1992. 215~219.
〔23〕许东禹,刘锡清,张训华,等.中国近海地质〔M〕.北京:地质出版社, 1997.54~143.
〔24〕陈丽蓉.渤海、黄海、东海沉积物中矿物组合的研究〔J〕.海洋科学, 1989, 13(2): 1~8.
〔25〕申顺喜,陈丽蓉,李安春,等.南黄海冷涡沉积和通道沉积的发现〔J〕.海洋与湖沼, 1993, 24(6): 563~570.
〔26〕Yang Z, Saito Y, Guo Z,et al. Distal mud area as a material sink in the East China Sea: global Fluxes of carbon and its related substances in the coastal sea-ocean-atmosphere system〔A〕. Proceedings of the 1994 Sapporo IGBP Symposium STA〔C〕. 1994. 1~6.
〔27〕赵松龄.陆架沙漠化〔M〕.北京:海洋出版社, 1996.124~130.
〔28〕莱尔曼A.湖泊的化学、地质学和物理学〔M〕.王苏民等译.北京:地质出版社, 1989.159~183.
〔29〕Athy L F. Density, porosity and compaction of sedimentary rocks〔J〕. AAPG Bull, 1930, 14: 1~24.
〔30〕Hedberg HD. Gravitional compaction of clays and shales〔J〕.American Journal of Science, 1936, 31: 241~287.
〔31〕魏永佩,陈会鑫.沉积盆地碎屑岩原始厚度恢复经验图版〔J〕.石油与天然气地质, 1999, 30(1): 90~93.
〔32〕Christensen E R. A model for radionuclides in sediments influenced by mixing and compaction〔J〕. Journal of Geophysical Research, 1982, 87: 566~572.
〔33〕Smith J N, Schafer C T. Bioturbation processed in continental slope and rise sediments delineated by 210Pb,microfossil and textual indicators〔J〕.Journal of Marine Research,1984, 42: 1 117~1 145.
〔34〕Mulsow S, Boudreau B P, Smith J N. Bioturbation and porosity gradients〔J〕. Limnology and Oceanography, 1998,43(1): 1~9.
〔35〕业渝光,和杰,刁少波,等.现代黄河三角洲Zk226孔岩石210Pb、Al、Fe、Mn、Cu的地球化学〔J〕.海洋地质与第四纪地质, 1991, 11(4): 25~34.
〔36〕林茂福,杨绍深,李太俊,等.南黄海沉积物中某些金属元素的地球化学行为的探讨〔A〕.见:涂光炽,欧阳自远主编.地球化学进展〔C〕.贵阳:贵州科技出版社, 1996.74~79.

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