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月岩(70017—291)的热释光测定 被引量：1

DETERMINATION OF LUNAR SAMPLE BY THERMO- LUMINESCENCE TECHNIQUE
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摘要 The lunar sample (70017-291) has been examined using TL technique. Its natural TL glow curve has been established. The effective storage temperature and the sunning degree of this sample have been estimated by comparing ours with the results determined by Dr. S. A. Durrani. The lunar sample (70017-291) has been examined using TL technique. Its natural TL glow curve has been established. The effective storage temperature and the sunning degree of this sample have been estimated by comparing ours with the results determin-ed by Dr. S. A. Durrani.
作者 刘京发 王维达
机构地区 不详 上海博物馆实验室
出处 《地球化学》 CAS 1980年第4期425-427,共3页 Geochimica
关键词 月球探测 岩石 微量元素 热释光测定
分类号 P184.5 [天文地球—天文学]
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同被引文献11

  • 1李虎侯.马兰黄土的热释光年龄(Ⅳ)——斋堂剖面的研究[J].地球化学,1990,19(3):264-269. 被引量：6
  • 2MacDiarmid R A. The application of thermoluminescence to geothermometry[J]. Econ Geol, 1963, 58(8): 1218-1228.
  • 3Azorin J. Determination of thermoluminescence parameters from glow curves - Ⅰ. A review[J] . Int J Radiat Appl Instrum Nucl Tracks Radiat Meas, 1986, 11(3): 159-166.
  • 4Chen R. Kinetics of TL glow peaks[M]//Horowitz Y S. Thermoluminescence and Thermoluminescent Dosimetry. Boca Raton: CRC Press, 1984:49 - 88.
  • 5Berger G W, Mulhern P J, Huntley D J. Isolation of silt-sized quartz from sediments[J]. Ancient TL, 1980 ( 11 ): 8 - 9.
  • 6Murray A S, Wintle A G. Application of the single-aliquot regenerative-dose protocol to the 375% quartz TL signal[J]. Radiat Meas, 2000, 32(5/6): 579-583.
  • 7Armstrong P A. Thermochronometers in sedimentary basins[J]. Rev Mineral Geochem, 2005, 58 ( 1 ): 499 - 525.
  • 8Chaillou D, Chambaudet A. Isothermal plateau method for apatite fission-track dating[J]. Nucl Tracks, 1981, 5(1/2): 181 - 186.
  • 9Fission-track annealing in apatite: Track length measurements and the form of the Arrhenius plot[J] . Nucl Tracks Radiat Meas, 1985, 10(3): 323-328.
  • 10陈永亨,徐敏,黄荣才.吉林陨石的热释光剖面与母体宇宙暴露历史示踪[J].地球化学,2000,29(6):604-607. 被引量：1

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地球化学
1980年 第4期

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