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J-GLOBAL ID:200902134713054303   Reference number:00A0413828

Solubility and behavior of lead in green orthoclase (amazonite) from Broken Hill, New South Wales, Australia.

オーストラリア,ニューサウスウエールズ州ブロークンヒルから産する緑色正長石における鉛の固溶と挙動
Author (5):
Material:
Volume: 95  Issue:Page: 71-84  Publication year: Mar. 05, 2000 
JST Material Number: F0509A  ISSN: 0914-9783  Document type: Article
Article type: 原著論文  Country of issue: Japan (JPN)  Language: ENGLISH (EN)
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Thesaurus term/Semi thesaurus term
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JST classification
Category name(code) classified by JST.
Silicate minerals  ,  Geochemistry of lithosphere in general 
Reference (26):
  • Binns, R.A. (1964), Zones of progressive regional metamorphism in the Willyama Complex, Broken Hill district, New South Wales. J. Geol. Soc. Aust., 11, 283-330.
  • Binns, R.A. (1965), The mineralogy of metamorphosed basic rocks from the Willyama Complex, Broken Hill district, New South Wales. Part II. Pyroxenes, garnets, plagioclase and opaque oxides. Mineral. Mag., 35, 561-587.
  • Binns, R.A. (1968), Experimental studies of metamorphism at Broken Hill. In Broken Hill Mines—1968 (M. Radmanovich and J.T. Woodcock Eds.), 199-204. Melbourne, Australasian Inst. Min. Met.
  • Burnham, C.W. (1967), Hydrothermal fluids at the magmatic stage. In Geochemistry of hydrothermal ore deposits (H.L. Barnes Ed.), 34-76. New York, Holt, Rinehart and Winston.
  • Cech, F., Misar, Z. and Povondra, P. (1971), A green lead-containing orthoclase. Tschermaks Min. Petr. Mitt., 15, 213-231.
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