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我国南海海盆一块锰壳层的生长速度及某些地球化学特征

夏明 张承蕙

夏明, 张承蕙. 我国南海海盆一块锰壳层的生长速度及某些地球化学特征[J]. 沉积学报, 1983, 1(2): 131-142.
引用本文: 夏明, 张承蕙. 我国南海海盆一块锰壳层的生长速度及某些地球化学特征[J]. 沉积学报, 1983, 1(2): 131-142.
Xia Ming, Zhang Chenhui. RATE OF ACCRETION OF MANGANESE CRUST FROM THE SOUTH CHINA SEA BASIN AND ITS GEOCHEMICAL CHARACTERISTICS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 131-142.
Citation: Xia Ming, Zhang Chenhui. RATE OF ACCRETION OF MANGANESE CRUST FROM THE SOUTH CHINA SEA BASIN AND ITS GEOCHEMICAL CHARACTERISTICS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 131-142.

我国南海海盆一块锰壳层的生长速度及某些地球化学特征

RATE OF ACCRETION OF MANGANESE CRUST FROM THE SOUTH CHINA SEA BASIN AND ITS GEOCHEMICAL CHARACTERISTICS

  • 摘要: 锰结核是海洋中重要矿产资源,它的成因至今众说纷纭。测定锰结核(包括锰壳层)的生长速度,应用放射性元素及其同位素研究锰结核与周围环境的关系,对于探讨锰结核的成因十分重要。铀系方法,包括230Th231Pa234U230Th/232Th,在测定锰结核的生长
  • [1] (1)夏明等,袖系方法鉴定因际际准样结果,中国科学,(1979),8,792-7990

    (2}契尔登采夫,234U及其在地质学If1的应用。1975,原子能出版社,258.

    (3) Bender M.L.et al..Manganesc nodules:their evolution, Science.151(1966),3708, 325-328.

    (4) Bende M.L.,KU T.Land Broecker W.S.Accumulation rates of manganese in Pelagic sediments and nodules.Earth Planet.Sci.Lett.,8(1970),2,113一1-IS.

    (5)Guichard F.、Reyss J.L.and Yokoyama Y.Grovsth rales of manganese nod-ues measured with 10 Be and 26 Nature, 272(1978),155-156.

    (6)Immel R.,and Osmond J.K.Micromanganese nodules in deepsca sediments,Uranium一isotopic esidence for postdeposltionaf origin.Chemicul Geology,18(196),263-2.2,

    (7)Kaufman A .,The232Th concentration of surface ocean water.GeochimCosmochi m.Acfa, 33(1969),6,717-724.

    (8) Krishnaswami S.and Cochran J.K.,Uranium and thorium series nuclides in oriented ferromanganese nodules:growth rates, turnov-er times and nu-elide behavior.Earth Planet.Sci.Lett.,40(1978),1,45-62.

    (9) Krishnaswami Sand Cochran J.K..Time Scales of Deep-Sea Ferromang-anew Nodulc Growth Based on 10Be and Alpha Trach Distributions and their Relation to Urrznium Decac Series Measurements.CoIIoque Inte-rnutional du C.N.R.S(1978),No.289, 1一13.

    (10)Ku T.L .U ranium series disequilibrium in deep sediments.Ph.D.thesis Columbia Universitv, New- York, 157.

    (11) Ku T.L.and Broeckcr N.S.Uranium,thorium and protactinium in a man-ganese nodule.Earth Planei.Sci.Left, 2(196i),317-320.

    (12)Ku T. L.,Radiochemical studies on manganese nodules of deep-sea origin.Deep-Soa Research, 16(1969),625-637.

    (13)Ku T.L.Rates of accretion.In marine Manganesc Deposits(1977)(ed.G.P.Glasl,),219-267 ,Elsevier,N.Y.

    (14)Ku T.Land Hnauss Iv.G.Radioactive disequiliorium in fissure一filling ma-terial and its implication in dating of manganese nodules.Colloque Intern-ational du C.N.R.S.No,289, sur la Genese des Nodules de Manganese,1979,Gif一Sur-Yvette, 289一293.

    (15)Ku T.L.,Omura A.and Chen P.S.10Be and U一series isotopes in Manganese Nodules from the central Vorth Pacific,Marine Geology and Oceanography of the Pacific ?Manganese Vodule Frovince,1979.(ed.Brischoff J.L.).791-814.

    (16)Laloa C.,Ku T.L.,Brichet E.et al.,TECHNO Encrustation Part 1:Radiometric studies. Colloque International du C.V.R.S.No.289, La Genese des Vodules de Manganese, 1979, 261一268.

    (17)Moore W.S.,The thorium isotope content ofoceanwater.Earth Planet.Sci.Lett.,53(1981),3,417一926.

    (18)Кузнецов Ю.В.Радцохрнодогця Океана.1976,Атомцздат,280.

    (19)Чердынцев В.В.Ц ДР,Происхожцеие железо-марганцевых конкреций Тпхого Океана по данным о раднонзотопах. Геохимня,(1971).3,339-354.
  • [1] 周伟, 王亚东, 袁四化.  东昆仑山新生代初始广泛隆升始于约20 Ma ——低温热年代学的证据 . 沉积学报, 2025, (): -. doi: 10.14027/j.issn.1000-0550.2025.012
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出版历程
  • 收稿日期:  1982-07-16
  • 刊出日期:  1983-06-10

目录

    我国南海海盆一块锰壳层的生长速度及某些地球化学特征

    摘要: 锰结核是海洋中重要矿产资源,它的成因至今众说纷纭。测定锰结核(包括锰壳层)的生长速度,应用放射性元素及其同位素研究锰结核与周围环境的关系,对于探讨锰结核的成因十分重要。铀系方法,包括230Th231Pa234U230Th/232Th,在测定锰结核的生长

    English Abstract

    夏明, 张承蕙. 我国南海海盆一块锰壳层的生长速度及某些地球化学特征[J]. 沉积学报, 1983, 1(2): 131-142.
    引用本文: 夏明, 张承蕙. 我国南海海盆一块锰壳层的生长速度及某些地球化学特征[J]. 沉积学报, 1983, 1(2): 131-142.
    Xia Ming, Zhang Chenhui. RATE OF ACCRETION OF MANGANESE CRUST FROM THE SOUTH CHINA SEA BASIN AND ITS GEOCHEMICAL CHARACTERISTICS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 131-142.
    Citation: Xia Ming, Zhang Chenhui. RATE OF ACCRETION OF MANGANESE CRUST FROM THE SOUTH CHINA SEA BASIN AND ITS GEOCHEMICAL CHARACTERISTICS[J]. Acta Sedimentologica Sinica, 1983, 1(2): 131-142.
    参考文献 (1)

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