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龙泉镁质闪石的拓扑交生 被引量:2

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摘要 一、龙泉镁质闪石的产出地质环境及一般特征 本文研究的镁质闪石呈束状或纤维状集合体,分布在龙泉构造混杂岩带的橄榄岩块周围.晶体长度从数毫米至1厘米左右.偏光显微镜下斜消光,C∧Ng=10°—13°;并见橄榄石、
出处 《科学通报》 EI CAS CSCD 北大核心 1991年第6期443-446,共4页 Chinese Science Bulletin
基金 国家教委博士点基金
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  • 1Thompson J B Jr. Geometrical possibilities for amphibole structure: Model biopyriboles. Amer Mineral, 1970, 55 (1-2): 292~293
  • 2Thompson J B Jr. Biopyriboles and Polysomatic series. Amer Mineral, 1978 (3-4), 63: 239-249
  • 3Thompson J B Jr. An introduction to the mineralogy and Petrology of biopyriboles. In: Reviews in Mineralogy. Washington DC: The Mineralogical Society of America, 1981, 9A: 141~185
  • 4Veblen D R, Burnham C W. New biopyriboles from Cherster, Vermont: Descriptive mineralogy. Amer Mineral, 1978, 63(9-10): 1000~1009
  • 5Veblen D R, Burnham C W. New biopyriboles from Cherster, Vermont: The crystal chemistry of jimthompsonite, clinojimthopsonite, and chesterite, and the amphibole-mica reaction. Amer Mineral, 1978, 63(11-12): 1053~1073
  • 6Veblen D R, Buseck P R. Chain-width order and disorder in biopyriboles. Amer Mineral, 1979, 64 (7-8): 687~700
  • 7Veblen D R, Buseck P R. Microstructures and reaction mechanisms in biopyriboles. Amer Mineral, 1980, 65 (7-8): 599~623
  • 8Veblen D R, Buseck P R. Hydrous pyriboles and sheet silicates in pyroxenes and uralites: Intergrowth microstructure and reaction mechanisms. Amer Mineral, 1981, 66 (11-12): 1107~1134
  • 9Veblen D R. Non-classical pyriboles and polysomatic reaction. In: Reviews of Mineralogy. Washington DC: The Mineralogical Society of America, 1981, 9A: 223~230
  • 10Nakajima Y, Ribbe P H. Texture and structure interpretation of the pyroxene to other biopyriboles. Contrib Mineral Petrol, 1981, 78 (3): 230~239

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