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原生金刚石矿床的构造控制:对选区的意义 被引量:1

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出处 《国外地质科技》 1995年第7期6-13,共8页
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  • 1宋国明.博茨瓦纳矿业开发与投资环境[J].国土资源情报,2006(5):21-25. 被引量:7
  • 2McDonald K S V. Platinum-group element geochemistry of mantle eclogites: a reconnaissance study of xenoliths from the Orapa kimberlite, Botswana[J].Applied Earth Science, 2006, 115(3): 81-93.
  • 3Matthew Field, Johann Stiefenhofer, Jock Robey, et al. Kim- berlite-hosted diamond deposits of southern Africa: A review[J]. Ore Geology Reviews, 2008, 34: 33-75.
  • 4Field M G, Gibson J, Wilkes T A, et al. The geology of the Orapa A/K1 kimberlite Botswana: further insights into the emplacement ofkimberlite pipes[J]. Russian Geology and Geo- physics, 1997, 38 (1):24-39.
  • 5Gernon T M, Fontana G, Field M, et ak Mac Niocaill. Pyro elastic flow deposits from a kimberlite eruption The Orapa South Crater, Botswana[J]. Lithos, 2009, 112:566- 578.
  • 6Viljoen K S, Smith C B, Sharp Z D. Stable and*radiogenic iso- tope study of eclogite xenoliths from the Orapa kimberlite, Botswana[J]. Chemical Geology, 1996,131 : 235 - 255.
  • 7Burgess R, Kiviets G B, Harris J W. Ar-Ar age determina- tions of eclogitic clinopyroxene and garnet inclusions in diamonds from the Venetia and Orapa kimberlites[J]. Lithos, 2004, 77: 113-124.
  • 8Stachel T, Viljoen K S, McDade P, et al. Diamondiferous lithospheric roots along the western margin of the Ka[ahari Craton-the peridotitic inclusion suitein diamonds from Orapa and Jwaneng[J]. Contrib Mineral Petrol, 2004, 147.. 32- 47.
  • 9Deines P, Harris J W, Gurney J J. Depth-related carbon isotope and nitrogen concentration variability in the mantle below the Orapa kimberlite, Botswana, Africa[J]. Geochimica et Cosmochimica Acta, 1993, 57:2781 -2796.
  • 10Deines P, Harris J W, Robinson D N, et al. Carbon and oxy- gen isotope variations in diamond and graphite eclogites from Orapa, Botswana, and the nitrogen content of their diamonds [J]. Geochimica et Cosmochimiea Acta, 1991, 55:515 - 524.

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