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马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物

张德玉

张德玉. 马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物[J]. 沉积学报, 1993, 11(1): 111-120.
引用本文: 张德玉. 马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物[J]. 沉积学报, 1993, 11(1): 111-120.
Zhang Deyu. Clay Mineralogy of the Sediments Deposited Since the Pleistocene in the Mariana Trough and the West Philippine Basin[J]. Acta Sedimentologica Sinica, 1993, 11(1): 111-120.
Citation: Zhang Deyu. Clay Mineralogy of the Sediments Deposited Since the Pleistocene in the Mariana Trough and the West Philippine Basin[J]. Acta Sedimentologica Sinica, 1993, 11(1): 111-120.

马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物

详细信息
    作者简介:

    张德玉,男,42岁,助理研究员,海洋沉积学及粘土矿物学.

Clay Mineralogy of the Sediments Deposited Since the Pleistocene in the Mariana Trough and the West Philippine Basin

  • 摘要: 根据三个沉积岩芯的研究,马里亚纳海槽和西菲律宾海盆更新世以来的沉积物中粘土矿物明显不同:前者以海槽内基性火山物质蚀变形成的蒙皂石为主,伴随少量铁镁绿泥石和伊利石;后者以来自海盆以西陆上岩石风化形成的伊利石为主,其次为蒙皂石、普通绿泥石和高岭石。这种差别除与物源有关外,主要与两个海盆中的火山活动有关。海槽内粘土矿物也有差异,迷可能与海底热液活动的影响有关。古气候对粘土矿物也有影响,但在海槽则被频繁的火山活动所掩盖。
  • [1] (1) Kolla, V., Nadler, L.及Bonatti, E., 1980, Clay mineral distributions in surface sediments of the Philippine sea. Oceanologica Acta, vol. 3, p.245-250

    (2) Latouche, C.& Maillet. N., 1982. X-ray mineralogy studies. Deep Sea Drilling Project Leg 60. In: Hussonf, D.M.et al.. (eds) Initial Reports of DSDP, vo1.60. p.437-453

    (3) Nagel. U.&Schumann, D.,1982. Mineralogy of sediments cored during Deep Sea Drilling Project Legs 58-60 in the north and south Philipping Sea: Results of X-ray diffraction analyses. In: Hussong, D. M. et al., (eds) Initial reports of DSDP. vol. 6U, p.415-435

    (4) Chamley, H.,1980. Clay sedimentation and paleoenvironment in the Shikoku Basin since the Middle Miocene, (Deep Drilling project, Leg 58, North Philippine Seal. Initial reports of DSDP, vol. 58, p.669-678

    (5) Desprairies, A.,1981, Authigenic minerals in volcanogenic sediments cored during Deep Sea Drilling Project Leg 60. In: Hussong, D. M. et al. (eds),Initial reports of DSDP. Vo1.60, p.455-465

    (6) Biscaye, P. E. 1965, Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans. Am. Geol. Soc. Bull., vo1.76, p.803-832

    (7) Brindley. G. W & Brown, G.,1980, crystal stuctures of clay minerals and their X- ray identification Mineralogical Society, London, P.495

    (8) Sudo, T.&Shimoda, S.,1978, Clays and clay minerals of Japan. Development in Sedimentology. 26 Amsterdam, p.20-70

    (9) Russell. J. D.& Clark, D. R., 1978. The effect of Fe for Si substitution on the b-dimension of nontronite. Clay M inerals, vo1.13, p.133-13'1

    (10) Copeland, R.A, et al., 1971, origin of clay minerals in a Mid-Atlantic Ridge sediments. Earth Planet. Sci. Letl vo1.10, p.133-137

    (11) Karig, D. E.,1975, Basin genesis in the Philippine Sea. In: D. K. Karig, et al.(eds.),Initial reports of DSDP, vo1.31,p.857-880

    (12) Alt, J. C.&Honnorez, J., 1984, Alteration of the upper oceanic crust. DSDP sUe 417: Mineralogy and them-istry. Contrib. Mineral Petrol., vo1.87, p.149-169

    (13) Londale. p.&Hawkins, J.,1985,Silicic volcanism at an off-axis geothermal Geld in the Mariana Trough back-arc basin. Am. Geol. Soc. Bull., vo1.96, p.940-951

    (14) Abbott, D. H.. Menke, W.&Morin, R., 1983, Constrains upon water advection in sediments of the Mariana Trough. J. Geophys. Res., vo1.88, p.1075-1093.
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出版历程
  • 收稿日期:  1990-04-12
  • 刊出日期:  1993-03-10

目录

    马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物

      作者简介:

      张德玉,男,42岁,助理研究员,海洋沉积学及粘土矿物学.

    摘要: 根据三个沉积岩芯的研究,马里亚纳海槽和西菲律宾海盆更新世以来的沉积物中粘土矿物明显不同:前者以海槽内基性火山物质蚀变形成的蒙皂石为主,伴随少量铁镁绿泥石和伊利石;后者以来自海盆以西陆上岩石风化形成的伊利石为主,其次为蒙皂石、普通绿泥石和高岭石。这种差别除与物源有关外,主要与两个海盆中的火山活动有关。海槽内粘土矿物也有差异,迷可能与海底热液活动的影响有关。古气候对粘土矿物也有影响,但在海槽则被频繁的火山活动所掩盖。

    English Abstract

    张德玉. 马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物[J]. 沉积学报, 1993, 11(1): 111-120.
    引用本文: 张德玉. 马里亚纳海槽和西菲律宾海盆更新世以来沉积物中的粘土矿物[J]. 沉积学报, 1993, 11(1): 111-120.
    Zhang Deyu. Clay Mineralogy of the Sediments Deposited Since the Pleistocene in the Mariana Trough and the West Philippine Basin[J]. Acta Sedimentologica Sinica, 1993, 11(1): 111-120.
    Citation: Zhang Deyu. Clay Mineralogy of the Sediments Deposited Since the Pleistocene in the Mariana Trough and the West Philippine Basin[J]. Acta Sedimentologica Sinica, 1993, 11(1): 111-120.
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