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Volume 5,Issue 4,1986 Table of Contents

   
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Contents

Discovery of Well一reserved Ophiolite and Its Basical Characters in Southeastern Margin of the Jiangnan Ancient Continent
  白文吉,甘启高,杨经绥,邢凤鸣,徐祥
  1986,5(4):289-299 [Abstract]  [View PDF(6.25 M)]
  
The Origin of the Spilite一keratophyre Series and the Characteristic of the Related Mantle一derived Granitic Rocks in Xiqiu Zhejiaag
  祁岖,周新民,王德滋
  1986,5(4):299-308 [Abstract]  [View PDF(4.48 M)]
  
The Characteristics and Origin of Uranium-bearing Silicious Limestones in the Western Section of the South Qinling
  黄振宇
  1986,5(4):309-315 [Abstract]  [View PDF(4.29 M)]
  
A Study on the Rare "Burned Kaolinite Clay Rock",in Northern Shanxi
  真允庆
  1986,5(4):315-322 [Abstract]  [View PDF(3.26 M)]
  
Petrological and Geochemical Charcteristcs and Forming Conditions of Genetic Types of Granites in Daguzhai-Luobuli
  郑永飞,张祖还,沈渭洲
  1986,5(4):323-331 [Abstract]  [View PDF(4.04 M)]
  
A Study of Modulated Structures and Complex Structures in Natural Alkali Feldspars:IV.Studies on Complex Structures of Alkali Feldspars of Volcaniclastic Rocks in the Northeast Part of Jiangxi Province
  彭志忠,廖立兵,西门露露
  1986,5(4):332-343 [Abstract]  [View PDF(8.59 M)]
  
经国际矿物协会(IMA)新矿物与矿物命名委员会批准1985—1986年发表的
  郭宗山,罗谷风,关雅先,王濮
  1986,5(4):344-345 [Abstract]  [View PDF(918.71 K)]
  
119Sn and 57Fe Mossbauer Studies of the Franckeite from Dachang
  吴功保,黄民智
  1986,5(4):346-352 [Abstract]  [View PDF(2.96 M)]
  
Simulating Experiment on the Conditions of Formation of Globular Uraninite
  沈才卿,赵凤民
  1986,5(4):353-362 [Abstract]  [View PDF(5.79 M)]
  
Oxygen Isotope Compositions of Metamorphic Minerals and Their Equilibrium Fractionation Temperatures in the Chencai Group,Zhejiang Province
  徐步台
  1986,5(4):362-367 [Abstract]  [View PDF(2.90 M)]
  
Guinier-Type Focusing Camera-an X一Kay Diffraction Device with High Resolution
  魏明秀
  1986,5(4):368-375 [Abstract]  [View PDF(3.89 M)]
  
A New Method of Determining the Alkalinity of Igneous Rock Series
  王希渠
  1986,5(4):376-378 [Abstract]  [View PDF(1.49 M)]
  
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