Prismatine含义的变化及其在南极中山站区的产出
Occurrence of prismatine at the Zhongshan Station area, East Antarctica, and the changes of its definition
-
摘要: 本文对prismatine(Prs)名称的来历作了简要介绍,指出kornerupine(Krn)系列中一个四面体位置上的B含量可变化于0和1之间(在22(O,OH,F)的分子式中),并伴随成分、晶体结构及矿物组合的变化。以 B=0.5为界划分可出两种不同的矿物:若B<0.5,为Krnss,包括两种情形:B=0,为无B之Krnss,0Abstract: A brief history of the name prismatine has been given in the paper. It is pointed out that the B content in one of thetetrahedrals of kornerupine varies between 0 and 1 (per formula unit of 22 (O, OH, F) ), being accompanied by the changingmineralogical properties such as composition, crystal structure and mineral association at its occurrence. Two distinct minerals aredefined by the critic of B = 0. 5, i. e., kornerupine sensu stricto (Krnss) if B 0. 5. Accordingly, the analogue (B = 0. 89) near Zhongshan Station of China at East Antarcticais prismatine which is unique in its abundance and occurrence even in the world. The corresponding Chinese names of the mineralsare recommended.
-
Key words:
- Prismatine /
- Kornerupine /
- Mineral name
[1] ［1］Carson CJ, Hand M and Dirks P H G M. 1995. Stable coexistence of grandidierite and kornerupine during medium pressure granulite facies metamorphism. Mineral. Mag., 59:327-339.
[2] ［2］Friend C R L. 1995. Occurrence of boron-free and boron-poor kornerupine. Mineral. Mag. , 59:163 -6
[3] ［3］Goβner B and Muβgnug F. 1928. Vergleichende rontgenographische Untersuchung von Magnesiumsiliken. Neues Jahrb. Mineral. , Geol.U. Pal ont., Abt. A, 58: 213-252.
[4] ［4］Grew E S, Yates M G and Marquez N. 1987. Boron-bearing kornerupine from Fiskenaesset, West Greenland: a re-examination of specimens from the type locality. Mineral. Mag. , 51: 695 -708.
[5] ［5］Grew E S. 1986. Petrogenesis of komerupine at Waldheim (Sachsen),German Democratic Republic. Zeits. Geol. Wissenschaften, 14:525 - 558.
[6] ［6］Grew E S, Chernosky J V, Werding G, Abraham K, Marquez N and Hinthorne J R. 1990. Chemistry of kornerupine and associated minerals, a wet chemical, ion microprobe, and X-ray study emphasizing Li, Be, B and F contents. Journal of Petrology, 31:1025 - 1070.
[7] ［7］Grew E S. 2002. Borosilicates and boron in rock-forming minerals in metamorphic environments. In: E S Grew & L M Anovitz ( eds. ).BORON Mineralogy, petrology and geochemistry. Reviews in Mineralogy, 33(2nd edition), 387 -502, Mineralogical Society of America.
[8] ［8］Grew E S, Cooper M A and Hawthorne F C. 1996. Prismatine:revalidation for boron-rich compositions in the kornerupine group.Mineral. Mag. , 60:483 -491.
[9] ［9］Jiang J. 1992. Main stage metamorphism and evolution of the khondalites in Mashan group. Acta Petrologica et Mineralogics, 11 (2) , 97 -110 (in Chinese with English abstract).
[10] ［10］Klaska R, and Grew E S. 1991. The crystal structure of boron-free kornerupine: Conditions favoring the incorporation of variable amounts of B through substitution in kornerupine. American Mineral, 76: 1824 - 1835.
[11] ［11］Lacroix A and de Gramont A. 1919. Sur la présence du bore dans quelques silico-aluminates basiques naturels. Comptes Rendus Acad. Sci. Paris,168:857 -861.
[12] ［12］Lorenzen J. 1886. Untersuchungen gronlandischer Mineralien. Zeitschrift für Kristallographie und Mineralogie, 11: 315 - 318.
[13] ［13］Moore P B and Araki T. 1979. Kornerupine: a detailed crystal-chemical study. Neues Jahrb. Mineral. Abh., 134:317-336.
[14] ［14］Ren L, Zhao Y, Liu X and Chen T. 1992. Re-examination of the metamorphic evolution of the Larsmann Hills, East Antarctica. In:Y. Yoshida, K. Kaminuma, and K. Shiraishi, (eds.). Recent Progress in Antarctic Earth Science, 145 - 153, Terrapub, Tokyo.
[15] ［15］Rotzler J, Hagen B and Hornes S. 1995. Evidence for ultra-high temperature/high pressure metamorphism in the Saxonian Granulite Massif, G ermany. Metamorphic Studies Group, Mineralogical Society of Great Britain and Ireland and Geological Society of London, Research in Progress and Annual General Meeting,Programme and Abstracts, p. 9.
[16] ［16］Sauer A. 1886. über eien eigenthumliche Granulitart als Muttergestein zweier neuer Mineralspecies. Zeits. Deutschen Geologischen Gesellschaft, 38:704-706.
[17] ［17］Stüwe K, Braun HM and Peer HM and Peer H. 1989. Geology and Structure of the Larsemann Hills area, Prydz Bay, East Antarctica.Australian Journal of Earth Sciences, 36: 219 - 241.
[18] ［18］Ussing N V. 1889. XXXIV. Untersuchungen der Mineralien von Fiskernas in Gronland. Zeits. Krist. Mineral., 15:596-615.
[19] ［19］Wang P, Pan Z and Wong L. 1984. Systematic Mineralogy(2), 224,Beijing: Geological Publishing House( in Chinese).
[20] ［20］Waters D J and Moore J M. 1985. Kornerupine in Mg-Al-rich gneisses from Namaqualand, South Africa: mineralogy and evidence for latemetamorphic fluid activity. Contrib. Mineral. Petrol., 91: 369-382.
[21] ［21］Werding G and Schreyer W. 1978. Synthesis and crystal chemistry of kornerupine in the system MgO - Al2 O3 - SiO2 - B2 O3 - H2O.Contrib. Mineral. Petrol. , 67: 247 -259.
[22] ［22］Werding G and Schreyer W. 2002. Experimental studies on borosilicates and selected borates, In: E. S. Grew & L. M. Anovitz(eds. ).BORON Mineralogy, petrology and geochemistry. Reviews in Mineralogy, 33 (2nd ed. ), 117 -164, Mineralogical Society of America.
[23] 姜继圣.1992.麻山群孔兹岩系主期区域变质作用及其演化.岩石矿物学杂志,11(2):97-110
[24] ［24］王濮,潘兆橹,翁玲宝.1984.系统矿物学(中册).北京:地质出版社,p.224
点击查看大图
计量
- 文章访问数: 6140
- PDF下载数: 5863
- 施引文献: 0
下载: