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电子探针分析(EPMA)在矿物学研究中的应用 被引量:1

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作者 毛水和
出处 《地质实验室》 1991年第2期118-128,共11页
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  • 1周剑雄 陈克樵.锆石Th-U-Pb等时年龄的电子探针测定的研究简介[J].国外矿床地质,1996,2:120-122.
  • 2Cocherie A,Legendre O.,Peucat JJ,et al.1998.Geochronlogy of polygenetic monazites constrained by in situ electron microprobe Th-U-Total lead determination:Implication for lead behaviour in monazite[J].Geochimica et Cosmochinica Acta, 62,(14):2475~2497.
  • 3Cocherie A,Albarede F.2001.An improved U-Th-Pb age calculation for electron microprobe dating of monazite.Geochimica et Cosmochimica Acta, Vol.65,(24):4509~4522.
  • 4Pommier A,Cocherie A.,Legendre O.2003."EPMA DATING":A program for Age calculation from electron microprobe measurements of U-Th-Pb.Geophiysical Research Abstracts,5,09054.
  • 5Braun I, Montel J M, Nicollet C. 1998. Electron Microprobe Dating of Monazites from High-Grade Gneisses and Pegmatites of the Kerala Khondalite Belt, Southern India[J]. Chem geol,146:65~85.
  • 6Suzuki K, Adachi M, Tanaka T.1991.Middle Precambria of Jurassic sand-stone in the Mino Terrane, central Japan: Th-U-total Pb evidence from an electron microprobe monazite study[J]. Sedimentary Geology, 75: 141~147.
  • 7Montel J M, Foret S, Veschambre M, et al.1996. Electron Microprobe Dating of Monazite[J]. Chem Geol, 131:37~53.
  • 8Rhede D, Wendt I, Forster H J.1996.A Three-Dimensional Method for Calculationg Independent Chemical U/Pb and Th/Pb-Ages of Accessory Minerals[J].Chem Geol, 130:247~253.
  • 9Suzuki K,Adachi M.1991a.Precambrian Provenance and Silurian Metamorphism of the Tsubonosawa Paragneiss in the South Kitakami Terrene,Northeast Japan [J].Geochem J,25:357~376.
  • 10Williams M, Jercinovic M, Terry M.1999. Age Mapping and Dating of Monzaite on the Electron Microprobe: Deconvoluting Multistage Tectonic Histories[J]. Geology, 27: 1023~1026.

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