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本文评述了热释光断代的近况。A review on the thermoluminescence dating is presented.
讨论了热释光剂量测量的质量控制问题。The quality control of thermoluminescence dosimetry is discussed.
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对冰洲石120℃热释光峰的基本特性进行初步研究。The basic characteristic of 120 ℃ thermoluminescence peak of iceland spar was studied.
在实验升温速率增大情况下，该峰值将向高温区移动。The thermoluminescence peak moves to the high temperature when the heating speed increasing.
土壤天然热释光法是一种能达到攻深找盲的方法，而且它的异常重复性很好。Natural soil thermoluminescence survey whose repeatability is very good can be used in exploring deep deposit.
第四纪沉积物天然热释光测量是一种累积间接油气勘查新方法。The measurement of natural thermoluminescence of Quaternary sediment is a new method for oil and gas prospecting.
如果晶体被加热，部份能量会以可见光的形式释放出来，这种现象叫做热释光现象。When such crystal is heated, the stored energy will be released as light, the so called thermoluminescence effect.
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数理统计分析结果表明沉积物的热释光和气烃的异常值完全吻合。The result of statistical analysis shows that the anomaly of thermoluminescence coincides well with methane anomaly.
绿柱石的热释光强度和峰温可作为其标型特征之一。The thermoluminescence strengths and peak temperatures of beryls can be regarded as the typomorphic characteristics.
本文叙述用细粒技术和粗粒石英技术研究热释光测定年代的方法。This paper describes the thermoluminescence dating method by using the fine grain and the quartz inclusion techniques.
石英热释光的发光曲线特征揭示了铀矿脉形成的热历史。The thermoluminescence patterns of quartz revealed clearly the thermal history during the formation of the uranium veins.
第四纪沉积物的天然热释光中储存有自沉积以来的累积辐射剂量。The natural thermoluminescence in Quaternary sediment has stored accumulated irradiated dose since the sediment deposited.
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土壤天然热释光测量是一种穿透能力较强的核技术方法，能探测到地下较深处的地球物理信息。Soil natural thermoluminescence surveying is an accumulation method of measuring radon and it can measure radon in a long time.
含金石英热发光曲线以双峰、三峰为特征而区别于不含金石英。The gold-bearing quartz can be distinguished from the gold-free quartzby its double, or triple peaks on the thermoluminescence curves.
结论GR-200A热释光探测器在医用高能电子线剂量测量中有一定的实用价值。Conclusion The practical value of GR-200A thermoluminescence detector is embodied in measurement of medical high energy electronic dose.
随成矿作用的演化，石英的热发光峰温趋于降低，发光强度趋于增加。Withthe evolution of ore-forming process, the peak temperatures tend to de-crease, and the thermoluminescence strengths tend to increase.
介绍了常规热释光个人剂量计IDB-2型的光子能量响应和最佳补偿方法。Photon energy response of Model IDB-2 routine thermoluminescence personal dosimeter and method of optimum compensation are given in this paper.
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油气藏上方天然辐射场和土壤样品中矿物组合的不均一性综合形成了土壤样品的天然热释光异常。The anomaly of soil natural thermoluminescence is caused by the differences of natural radiation and minerals in the sediment over oil reservoir.
简单介绍了土壤天然热释光方法测量原理，研究了土壤热释光测量的影响因素。The paper brief introduces the principle of the measurement of soil natural thermoluminescence and studies the factor that affect the survey results.
对不同剖面火山岩的热释光特征进行比较，可能确定其喷发期次而进行火山岩地层的对比。Comparing with thermoluminescence character of different volcanic rocks section, we will confirm eruptible stage to contrast in volcanic rocks stratum.