| 热释光断代技术测定断层活动时代可能性的研究 |
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| 引用本文： | 计凤桔,高平.热释光断代技术测定断层活动时代可能性的研究[J].地震地质,1988,10(4):207. |
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| 作者姓名： | 计凤桔 高平 |
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| 作者单位： | 国家地震局地质研究所
(计凤桔)，国家地震局地质研究所(高平) |
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| 摘 要： | 本文根据多年来研究断层活动所积累的热释光年龄资料和断层运动过程中各种温、压条件变化的模拟实验结果,阐述了断层运动所产生的摩擦升温有可能使断层面上乃至断层带内某些矿物原有的热释光“退火”,初步探讨了用热释光测年技术测定断层活动年代的可能性
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| 关 键 词： | 热释光断代 断层活动时代 摩擦升温 热释光退火 |
APPLICABILITY OF THERMOLUMINESCENT TECHNIQUE TO DATING OF FAULTING |
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| Ji Feng-ju and Gao Ping.APPLICABILITY OF THERMOLUMINESCENT TECHNIQUE TO DATING OF FAULTING[J].Seismology and Geology,1988,10(4):207. |
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| Authors: | Ji Feng-ju and Gao Ping |
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| Abstract: | Based on thermoluminescent age data accumulated for several years and the results of experiments at different P, T condition simulating faulting process, this paper states that the frictional heating caused by faulting may lead to the "annealing" of original ther-moluminescence of some minerals on the fault plane or even within the fault zone. The applicability of TL technique to dating episodes of faulting has been discussed as well. |
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| Keywords: | TL dating Ages of faulting Frictional heating TL annealing |
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