高级搜索

留言板

尊敬的读者、作者、审稿人, 关于本刊的投稿、审稿、编辑和出版的任何问题, 您可以本页添加留言。我们将尽快给您答复。谢谢您的支持!

姓名
邮箱
手机号码
标题
留言内容
验证码

河北卢龙武山寒武系—奥陶系界线粘土矿物研究

王宗哲 杨杰东

王宗哲, 杨杰东. 河北卢龙武山寒武系—奥陶系界线粘土矿物研究[J]. 沉积学报, 1985, 3(2): 57-66.
引用本文: 王宗哲, 杨杰东. 河北卢龙武山寒武系—奥陶系界线粘土矿物研究[J]. 沉积学报, 1985, 3(2): 57-66.
Wang Zongzhe, Yangjiedong. CLAY MINERALS FROM THE STRATA NEAR THE CAMBRIAN- ORDOVICIAN BOUNDARY SECTION AT WUSHAN OF LULONG, HEBEI PROVINCE[J]. Acta Sedimentologica Sinica, 1985, 3(2): 57-66.
Citation: Wang Zongzhe, Yangjiedong. CLAY MINERALS FROM THE STRATA NEAR THE CAMBRIAN- ORDOVICIAN BOUNDARY SECTION AT WUSHAN OF LULONG, HEBEI PROVINCE[J]. Acta Sedimentologica Sinica, 1985, 3(2): 57-66.

河北卢龙武山寒武系—奥陶系界线粘土矿物研究

CLAY MINERALS FROM THE STRATA NEAR THE CAMBRIAN- ORDOVICIAN BOUNDARY SECTION AT WUSHAN OF LULONG, HEBEI PROVINCE

  • 摘要: 河北卢龙武山寒武系—奥陶系界线剖面暴露良好、沉积连续、具有典型海相沉积特征以及丰富的古生物标准化石(如三叶虫和牙形刺等),因此该处受到许多地质研究人员的重视并被选为华北型寒武系—奥陶系界线层型剖面的地点。本文配合寒武系—奥陶系界线层型剖面的研究,对界线附近地层的粘土矿物进行了鉴定并探讨了古沉积环境。
  • [1] (1)Thorez.J.,1976,practical identification of clay minerals, G.L elotte,Ed. Dison,Belgique.

    (2)MaxwelI,D.T.and Hower, J.,1967,High-grade diagenesis and low-grade metam- orphism of illite in Precambrian Belt,Amer.Min.,52, 843-857。

    (3)Weaver,C.E.,1960,Possibld uses of clay minerals in search for oil,Bull. Am.Assoc. Geol.44,I505-1518.

    (4)Weaver,C.E.,1961,Clay minerals of the O nachita structural belt and adjacent foreland.in:the O nachita system,the U niv. T exeas Publ.,6120,Bureau Econ. Geol.Austin,147-160.

    (5)Dunoyer de Segonzac,G.,1969,Les mineraux argileux dans la diagenese- passage au metamorphisme,Mem.29,serv Carte Geols. Als Lorr.,320p.

    (6)Frey,M.,1970,The step from diagenesis to metamophism in pelitic rocks during Alpine Orogenesis,Sedimentology,15,261-279.

    (7)Post, J.L.,and Plummer,C.C.,1972, T he chlorite series of Flagstaff Hillarea,California:a preliminary investigaton,Clays and Clay Min.,20,271-283.

    (8)Johns,W.D.,Grim,R.E.and Bradley,W.F.,1954, Quantitative estimations of minerals by diffraction methods, J.Sed.Petrol,24, 242-251.

    (9)Brindley,G.W. and De Kimpe, C.,1961,Identification of clay minerals by single crystal electron diffraction,T he A m erican mineralogist,46,P1005.

    (10) Clauer,N.,1979, A ne w approach to Rb-Sr dating of sedimentary rock,In: E.Jager and J.C.Hunziker (Editors),L ectures in Isotope Geology,Springer- Verlag,Berlin, 30-51

    (11) Kisck,H.J.,1983,Mineralogy and petrology of burial diagenesis(burial metam-orphism) and incipient metamorphism in elastic rocks,In:G.,Larsen and G.V., Chilingar (Editors),Developments in Sedimentology 25R, Elsevier, 289-494.

    (12) White,W.A.,1961,Colloidal phenomena in sedimentation of argillaceous rocks, J .sediment.Petrol.,31,560-570.

    (13) Meade,R.H.,1966,E actors influencing the early stages of the co m paction of claps and sands-review,).Sediment.petrol.,36,1085-1101.
  • [1] 李忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, (6): 928-933.
    [2] 李 忠.  “从最高到最深”—从第17届国际沉积学大会看沉积学研究前沿 . 沉积学报, 2006, 24(06): 928-933.
  • 加载中
计量
  • 文章访问数:  558
  • HTML全文浏览量:  5
  • PDF下载量:  336
  • 被引次数: 0
出版历程
  • 收稿日期:  1983-08-29
  • 刊出日期:  1985-06-10

目录

    河北卢龙武山寒武系—奥陶系界线粘土矿物研究

    摘要: 河北卢龙武山寒武系—奥陶系界线剖面暴露良好、沉积连续、具有典型海相沉积特征以及丰富的古生物标准化石(如三叶虫和牙形刺等),因此该处受到许多地质研究人员的重视并被选为华北型寒武系—奥陶系界线层型剖面的地点。本文配合寒武系—奥陶系界线层型剖面的研究,对界线附近地层的粘土矿物进行了鉴定并探讨了古沉积环境。

    English Abstract

    王宗哲, 杨杰东. 河北卢龙武山寒武系—奥陶系界线粘土矿物研究[J]. 沉积学报, 1985, 3(2): 57-66.
    引用本文: 王宗哲, 杨杰东. 河北卢龙武山寒武系—奥陶系界线粘土矿物研究[J]. 沉积学报, 1985, 3(2): 57-66.
    Wang Zongzhe, Yangjiedong. CLAY MINERALS FROM THE STRATA NEAR THE CAMBRIAN- ORDOVICIAN BOUNDARY SECTION AT WUSHAN OF LULONG, HEBEI PROVINCE[J]. Acta Sedimentologica Sinica, 1985, 3(2): 57-66.
    Citation: Wang Zongzhe, Yangjiedong. CLAY MINERALS FROM THE STRATA NEAR THE CAMBRIAN- ORDOVICIAN BOUNDARY SECTION AT WUSHAN OF LULONG, HEBEI PROVINCE[J]. Acta Sedimentologica Sinica, 1985, 3(2): 57-66.
    参考文献 (1)

    目录

      /

      返回文章
      返回